用户名: 密码: 验证码:
北秦岭地体东段岩浆作用与地壳演化
详细信息    本馆镜像全文|  推荐本文 |  |   获取CNKI官网全文
摘要
北秦岭地体东段是秦岭造山带的重要组成部分,以复杂多样的岩石组成、多期次的构造岩浆作用、变质地体的相互叠置为特点,地体内不仅大量产出秦岭造山带中最古老的前寒武纪基底—秦岭群,而且广泛出露晋宁期和加里东-海西期的花岗闪长质侵入岩类,因而它既是探讨中国南北两大陆块(华南和华北)碰撞、拼合关系的关键位置,又是研究秦岭造山带地壳的形成和演化、花岗岩类的成因物源及其构造属性的最佳理想场所。为了较好地约束秦岭群的源区特征和构造背景,揭示北秦岭地体的岩浆作用和地壳演化规律,本文运用多种测试方法和分析手段,主要包括主、微量元素分析、全岩Rb-Sr和Sm-Nd同位素分析以及锆石原位U-Pb定年和O-Hf同位素测试等,重点研究了秦岭群基底片麻岩和角闪岩两种主要岩石类型、晋宁期和加里东-海西期花岗侵入岩类,尤其详细剖析了后者的岩石组合特征、时空分布规律,并对不同成因类型侵入岩的源区及岩石成因进行了系统讨论,最后建立了晋宁期和加里东-海西期岩浆作用的年代学格架,通过与其邻区华北南缘、南秦岭及扬子北缘地体岩浆作用和地壳演化的对比,系统总结了北秦岭地体地壳的生长和再造历史。研究结果不仅为岩石的成因提供可靠的数据支持和地球化学制约,而且有助于认识秦岭造山带基底的演化和构造的归属,对揭示岩浆形成的深部地球动力学背景和探索大陆碰撞造山过程中地壳的生长、分异和演化具有重要的科学意义。
     秦岭群主要由片麻岩、角闪岩和少量大理岩组成,记录了北秦岭地体形成和早期的陆壳演化过程,经历了多期变形和变质作用。其中,长英质片麻岩富集轻稀土元素和大离子亲石元素(Rb、Ba、Th、K和Pb),Eu负异常和亏损高场强元素(Nb, Ta, P, Ti),锆石δ18O值变化略大且位于6.5-9.3‰之间,全岩初始εNd值-4.6,两阶段Nd模式年龄TDM2=1.99Ga;斜长角闪岩也富集大离子亲石元素和轻稀土元素,且亏损Nb和Ta,锆石δ18O值均一为5.0-6.0‰,但具有较高的全岩初始ENd值(2.8~3.3)和较年轻的TDM2(1.29~1.24Ga)。锆石U-Pb年龄表明长英质片麻岩和斜长角闪岩均形成于~960Ma与火山弧相关的构造背景之中,而非前人所认为的裂谷环境,同时发现一期早古生代的变质热事件。秦岭群碎屑锆石年龄谱显示其可能为一个独立的地质单元,并在新元古代早期具有不同于南北两大陆块的演化历史,很可能为格林威尔造山带的一个残留体。
     晋宁早期(-940)的花岗岩侵入体在南秦岭地体中极为少见,在北秦岭地体中却出露相当广泛且几乎都经历了明显的变质变形作用,这些岩体记录了秦岭造山带前寒武纪基底地壳的形成和演化历史。本文选取方庄和德河两个岩体为代表。结果表明,方庄花岗质糜棱岩的锆石结晶年龄为933.4±9.2Ma,δ18O值8.3~11.9‰,初始87Sr/86Sr比值0.72455,初始εNd值-6.0,Nd模式年龄2.09Ga (TDM2);德河黑云斜长片麻岩的锆石结晶年龄为939.7+7.6Ma和948.1+8.9Ma,δ180值8.6~10.0‰,初始87Sr/86Sr比值变化较大为0.70986~0.72455,初始εNd值-5.3--4.8,Nd模式年龄2.05~2.00Ga(TDM2)。结合已报道的15个新元古代花岗岩类岩体的年龄和地球化学数据,北秦岭地体新元古代岩浆作用可以划分为980~870Ma挤压碰撞作用和~844Ma伸展裂解作用两大阶段,包括~940Ma强烈变形S型同碰撞花岗岩、-880Ma弱-无变形后碰撞Ⅰ型花岗岩和~844Ma板内A型花岗岩三类花岗岩体。地球化学组成显示,这些花岗岩类岩石可能源自不同时期形成的秦岭群基底杂岩的部分熔融,但在后碰撞阶段幔源物质或年轻地壳物质的加入明显增加。北秦岭地体中新元古代岩浆活动与Rodinia超大陆演化基本同时代,可能记录超大陆形成过程中的地壳响应。在新元古代之前,北秦岭地体或许具有不同于华北陆块和华南陆块的演化历史。
     加里东一海西期岩浆活动在北秦岭地体东段广泛发育,在其周缘地体中几乎未见出露。本文对研究区内共10个中酸性侵入体19件样品和中基性富水杂岩体中的4件样品进行锆石U-Pb定年分析。结合近期公开报道的53件锆石U-Pb年龄数据,建立和查明北秦岭地体东段加里东-海西期岩浆活动的年代学格架和时空分布特征,将该期岩浆活动划分为3个阶段:第一阶段(-487Ma),主要分布于研究区东部;第二阶段(-450Ma),遍布整个研究区;第三阶段(-417Ma),分布于研究区中部。
     第一阶段(-487Ma):Ⅰ型花岗岩以板山坪、西庄河及麻池河乡等岩体为代表,具有类似于俯冲洋壳成因埃达克质岩石的地球化学特征,具有较高的初始εNd值(0.19~3.17)、较低的初始87Sr/86Sr比值(0.70257~0.70524)、较高的初始εHf值(2.51~13.97)、TDM2(Nd)=0.92~1.21Ga和TDM2(Hf)=0.56~1.28Ga及相对低的全岩δ18O值(7.03-7.60‰),这些特征指示该阶段Ⅰ型花岗岩可能源自俯冲洋壳板片的部分熔融。结合空间上与之共生的岛弧成因的富水杂岩的产出,两种岩浆作用类型共同证实了研究区内早古生代板块俯冲-消减事件的存在。S型花岗岩以漂池和蛮子营岩体为代表,具有高硅、钾,低钛、镁的特征,属高钾钙碱性过铝质系列,其初始εNd值=-7.98~-10.05、初始87Sr/86Sr比值=0.70352~0.72737、初始εHf值=-13.75~-0.78、TDM2(Nd)=1.89~2.06Ga、TDM2(Hf)=1.46~2.33Ga、锆石δ180值较高位于7.88~8.65‰之间,略低于全岩618O值10.9-11.7‰,这些特征共同指示该S型花岗岩具有板块俯冲过程中诱发活动陆缘陆壳物质熔融成因特征。
     第二阶段(~450Ma):~460Ma I型花岗岩以灰池子岩体最为典型,具有加厚下地壳成因埃达克岩的地球化学特征,具有中等的初始εNd值(-0.51~1.54,多数大于0),较低的初始07Sr/86Sr比值(0.70463~0.70612),变化较大的初始EHf值(-10.89~12.80),TDM2(Nd)=1.08~1.25Ga和TDM2(Hf)=0.61~1.70Ga,全岩δ180值相对较高为7.60~9.08‰,这些特征结合继承锆石的大量出现和在岩体内部未见中基性暗色包体的地质事实共同指示该阶段Ⅰ型花岗岩可能是新生的加厚下地壳部分熔融的产物,其源岩物质与第一阶段Ⅰ型花岗岩基本类似,其形成背景与古生代期间商丹洋壳的俯冲-汇聚-碰撞,进而导致新生下地壳的缩短-叠置-加厚有关;-450Ma I-S型花岗岩,以五垛山、宽坪、枣园、黄柏岔及桃坪岩体为代表,岩体岩石兼具碰撞型和俯冲型岩石的成因特点,总体显示其成因及物源与-460MaⅠ型花岗岩相似,不同之处较前者富集Nd同位素和具有较高的全岩δ18O值(9.96-10.34‰),可能暗示了幔源物质的贡献相对早期较少;-440Ma Ⅰ型花岗岩以沿商丹缝合带分布的武关及小王涧岩体为代表,它们可能是造山过程中滞后的消减源区发生部分熔融的产物。S型花岗岩以安吉坪和土桥岗岩体为代表,具有类似于第一阶段中S型花岗岩的高钾钙碱性过铝质系列岩石的特征,其初始ENd值=-7.64~-8.20、高初始87Sr/86Sr比值=0.71025~0.71263、TDM2(Nd)=1.8l~1.88Ga、锆石δ18O值较高位于9.60~13.30%o之间,总体呈现挤压碰撞成因的岩石地球化学特点。
     第三阶段(-417Ma):Ⅰ型花岗岩以侵入于二郎坪群的张家庄岩体为代表。该岩体岩石具有低钾(Na2O/K2O=3.30~28.83)拉斑玄武岩系列过铝质的特点,其高初始εNd值=3.19~5.07、低初始87Sr/86Sr比值=0.70331~0.70471以及TDM2(Nd)=0.74~0.89Ga,这些地球化学和同位素特征可能是新元古代期间形成的新生底侵基性岩浆或早期就位于造山带根部的早期基性岩浆混染了较少量的古老壳源物质熔融所致;物源方面与形成于新元古代的北秦岭第一类基性火山岩有较好的亲缘关系,暗示新元古代晚期存在又一期新生地壳的生长事件。S型花岗岩以丹凤岩体为代表,总体显示高硅和钾、富碱、低镁等特点,稀土和微量元素显示陆壳重熔S型花岗岩的特征。
     总体上,三个阶段中的Ⅰ型花岗岩,其物源基本与南秦岭火山岩或北秦岭第一类基性火山岩有很好的亲缘性,与华北物质基本无关;而S型花岗岩的物源则主要来自秦岭群片麻岩、宽坪群变沉积岩以及北秦岭第二类基性火山岩,华北基底物质对其也无贡献。
     北秦岭地体东段地壳生长以幕式增生为主,主要形成于古-中元古代及新元古代。在~2300Ma和~2000Ma主要表现为古老地壳物质的再造,在~1600Ma、1000~630Ma及~500Ma以地壳的增生为主,同时兼具古老地壳物质的再循环。通过与邻区地壳演化过程对比发现,华北南缘发生显著地壳增生时代为中太古代(~2700Ma);北秦岭地体在中元古代以后才开始发生大规模的地壳生长;南秦岭地壳增生事件可能主要发生在新元古代;扬子北缘主要在太古代和中元古代发生大规模的地壳生长或再造。在这四个构造地体中,仅有北秦岭地体缺少太古宙时期地壳的生长或改造事件。因此,元古代之前(>2000Ma),北秦岭地体可能为一个独立的地质体,具有不同于华北南缘、南秦岭以及扬子北缘的独特地壳演化历史。
The North Qinling terrain, being an important part of Qinling orogenic belt, is characterized by diverse rocks, multiphase tectonic-magmatic-metamorphic events. This terrain is composed of not only basement rocks of the Qinling Group, but also numerous magmatic rocks in different ages of the Jinningian, Caledonian, and Hercynian periods. The Qinling Group is previously interpreted as the oldest Precambrian basement unit of the North Qinling Terrain. Therefore, North Qinling is a key location to reveal the relationship of collision and assemblage between the North and South China blocks, and also an ideal place to research formation and evolution of crustal terrains, genesis of granitoids and provenance of tectonic units.
     In order to better understand provenance and tectonic setting of the Qinling Group and to reveal magmatism and crustal evolution in the North Qinling terrain, a detailed study of major and trace elements and Rb-Sr and Sm-Nd isotopic composition of whole-rock samples, as well as U-Pb ages and Hf-O isotopic data of zircons from the same analytical spot by the SIMS and LA-MC-ICP MS techniques, was measured for different rocks collected from two major rock units of the Qinling Group (felsic gneiss and amphibolite) and granitoids (Jingningian, Caledonian and Hercynian periods) in eastern North Qinling. Rock associations and spatial-temporal distribution of the Jingningian and Caledonian-Hercynian magmatic rocks throughout North Qinling are investigated for petrogenesis, magma source, geochronological framework of different magmatic events. Further, by comparison with magmatism and crustal evolution of the adjacent areas, crustal growth and reworking in the North Qinling terrain are systematically summarized. Research results in this study not only place geochemical constraints on genesis of these rocks, but also provide insight into evolution of the basement and tectonic provenance of the Qinling orogenic belt, and further help to better understand geodynamic background during the formation and evolution of continental crust in orogenic processes.
     The Qinling Group consists predominantly of gneisses and amphibolites and minor marbles, and underwent multi-phase deformation and metamorphism. This geological unit records hence the formation and early crustal evolution of the North Qinling terrain. Felsic gneisses exhibit enrichment of LREEs and LILEs (Rb, Ba, Th, K, Pb), negative Eu-anomalies and depletion of HFSEs (Nb, Ta, P, Ti). The rocks have slightly elevated δ18O values (6.5~9.3‰) and initial εNd values of-4.6corresponding to two-stage Nd model age of1.99Ga. Amphibolites are also enriched in LILE and LREE and depleted in Nb and Ta, and have homogeneous δ18O values (5.0-6.0%o), but higher initiald values (2.8~3.3) and younger two-stage Nd model ages (1.29~1.24Ga) compared to the gneisses. These rocks were emplaced in a~960Ma volcanic arc environment rather than in a rift setting as previously suggested. A major metamorphic event took place in early Paleozoic. Based on the age spectrum of detrital zircons, the Qinling Group is interpreted as an independent geological unit, which was mainly derived mostly from1000~900Ma old granitoid rocks. The North Qinling terrain can be regarded as a remnant of the Grenville orogenic belt with an early Neoproterozoic evolution different from the North and South China blocks.
     Granitoids of Jingningian ages exposed both in the South and North Qinling terrains and record Precambrian crustal formation and evolution of the basements in the Qinling orogenic belt. However, Early Jingningian granitic intrusive are rare in South Qinling but numerous in North Qinling. In this study, the Fangzhuang and Dehe granitoid plutons emplaced into the Qinling Group in the North Qinling terrain are chosen as research object. Analytical results show that zircons of the Fangzhuang granite pluton formed in933.4±9.2Ma, zircons have δ18O values of8.3~11.9‰and whole-rock yields initial εNdd value of-6.0, Nd model age of2.09Ga (TDM2) and initial87Sr/86Sr ratio of0.7246, while zircons of the Dehe granite pluton crystallized in939.7±7.6Ma and948.1±8.9Ma and whole-rock has initial Nd values of-5.3~-4.8, corresponding to Nd model ages of2.05-2.00Ga (TDM2) and variable initial87Sr/86Sr ratios of0.7099~0.7246. Integrating with isotopic ages of fifteen Neoproterozoic granitoid plutons exposed within the North Qinling terrain previously reported, the Neoproterozoic magmatism in this terrain can be subdivided into two major stages resulted from980~870Ma compressional and~844Ma extensional tectonic settings, including granitoids of~940Ma syn-collisional,~880Ma post-collisional and~844Ma extensional origin. Geochemical and isotopic features of these granitoids indicate that they probably originated from partial melting mainly of crustal material similar to the Qinling Group, but contribution of mantle or juvenile material to the magmas became significant after~900Ma in the post-collisional processes. Neoproterozoic magmatic activities in the North Qinling terrain are broadly simultaneous with the formation of supercontinent Rodinia and hence, they record response of the basement in this terrain. The crustal evolution in North Qinling terrain prior to the Neoproterozoic was likely different from those in the North and South China blocks.
     Caledonian-Hercynian magmatic activities were extensively developed in the North Qinling terrain, but it is scarcely present in the adjacent terrains. In this study, nineteen samples from ten intermediate-acidic intrusions and four samples from the intermediate-basic Fushui complex in the North Qinling terrain were measured for zircon U-Pb ages using SIMS and LA-ICP MS techniques. Integrating with fifty-three zircon isotopic ages previously reported in North Qinling, a geochronologic framework can be established for spatial and temporal distribution of the Caledonian-Hercynian magmatism in this terrain. It can be subdivided into three major phases of granitoids:-487Ma mainly distributed in eastern part of the study area,~450Ma occurring throughout the study area, and~417Ma scattered only in middle part of the study area.
     Stage one (-487Ma):I-type granitoids in geochemical composition, represented by the Banshanping, Xizhuanghe and Machihexiang plutons, are similar to adakites related to subducted oceanic-crust. They have initial87Sr/86Sr ratios of0.7026~0.7052, high initial εNd values of0.19-3.17and young two-stage Nd model ages of0.92-1.21Ga, and δ18O values between7.03and7.60%o. Coexisting with the island-arc related Fushui complex in the terrain, two types of magmatism together confirm an Early Paleozoic subduction event, which points to this I-type granitoids may be derived from partial melting of subducted oceanic crust. S-type granitoids, particularly the Piaochi and Manziying plutons, have high SiO2and K2O contents and low TiO2and MgO contents and define a high-K calc-alkaline magma trend. They have initial87Sr/86Sr ratios of0.7035~0.7274, lower initial εNd values of-7.98~-10.05and two-stage Nd model ages of1.89~2.06Ga, and zircon δ18O values of7.88~8.65‰, lower than whole-rock δ18O values of10.9-11.7%o, likely indicating S-type granites resulted from melting of crustal material induced by the subduction.
     Stage two (-450Ma):I-type granitoids (-460Ma) represented by the Huichizi pluton is analogous to thickened lower crust derived adakitic rocks, which have initial87Sr/86Sr ratios of0.70463~0.70612, initial εNd values of-0.51~1.54and two-stage Nd model ages of1.08~1.25Ga and two-stage Hf model ages of0.61~1.70Ga, and whole-rock δ18O values between7.06and9.08%o. This type of plutons does not contain intermediate-basic magmatic enclaves but many inherited zircons, implying that granites might be products of partial melting of thickened juvenile lower crust, whose source is the same as I-type granites from Stage one and related to Paleozoic Sangdan oceanic crust subduction-converge-collision, resulting in juvenile lower crust shortened, superimposed and thickened. I-S-type granites (-450Ma), represented by the Wuduoshan, Kuanping, Zaoyuan, Huangbaicha and Taoping plutons, have some characteristics of both collision-related and subduction-related granitoids. They overall display similar feature and more enriched in Nd and O isotopic composition compared to I-type granite (-460Ma), indicating contribution of mantle-derived material is relatively less than the older granites. I-type granitoids (-440Ma), represented by the Wuguan and Xiaowangjian plutons distributed along the Shangdan suture zone, might be the product of partial melting of pre-existing crustal component in subduction zone. S-type granites represented by the Anjiping and Tuqiaogang plutons display a high-K calc-alkaline magma trend as the stage one, which have an initial87Sr/86Sr ratios of0.71025~0.71263, lower initiald values of-7.64~-8.20and two-stage Nd model age of1.81~1.88Ga, and zircon δ18O values of9.60~13.30‰, indicating feature of compression and collision origin.
     Stage three (-417Ma):I-type granitoids, represented by the Zhangjiazhuang pluton, display a low-K (Na2O/K2O=3.30~28.83), peraluminous tholeiite magma trend, and have lower initial87Sr/86Sr ratios of0.70331~0.70471, high initial εNd values of3.19-5.07, corresponding to two-stage model Nd age of0.74-0.89Ga, implying that another juvenile crustal growth may be occurred in late Neoproterozoic. Geochemical and isotopic features indicate that they probably originated from the partial melting of the underplating juvenile basic magma or magma that had already been emplaced into orogenic root during the early stage, mixing with small amounts of ancient crustal material. S-type granites, represented by the Danfeng pluton, have high SiO2and K2O contents and low MgO content. Their geochemical characteristics point to products of re-melting of continental crust.
     Overall, I-type granitoids of three stages originated from the sources closely related to basic volcanic rocks in the South and North Qinling terrains but irrelevant to the basement of North China. However, S-type granites were mainly derived from crustal material similar with metamorphic rocks of the Qinling and Kuanping Groups, without contribution of the basement of North China block.
     Crustal formation in the eastern North Qinling is characterized by episodic growth that mostly took place in Proterozoic through reworking of ancient crustal material at~2300Ma and2000Ma, crustal growth and recycling of ancient crust at-1600Ma,1000~630Ma and~500Ma, respectively. By comparison with the adjacent terrains, it can be observed that the North Qinling terrain can be interpreted as a separate geological entity with a special evolution different from the South and North China blocks before Proterozoic. Crustal growth in the southern margin of the North China block took place in Archean (~2700Ma), the South Qinling terrain mainly in Neoproterozoic and the northern margin of the Yangtze block in Archean and Mesoproterozoic, while the North Qinling terrain began massive growth after Mesoproterozoic.
引文
Amelin, Y., Lee, D. C., Halliday, A. N.2000. Early-middle archaean crustal evolution deduced from Lu-Hf and U-Pb isotopic studies of single zircon grains. Geochimica Et Cosmochimica Acta,64(24):4205-4225.
    Amelin, Y., Lee, D.-C., Halliday, A. N., Pidgeon, R. T.1999. Nature of the Earth's earliest crust from hafnium isotopes in single detrital zircons. Nature,399(6733):252-255.
    Andersen, T.2002. Correction of common lead in U-Pb analyses that do not report 204Pb. Chemical Geology,192(1-2):59-79.
    Atherton, M. P., Petford, N.1993. Generation of sodium-rich magmas from newly underplated basaltic crust. Nature,362(6416):144-146.
    Bader, T.2011. Multiple high-and ultra-high-pressure orogenies in the Qinling Mountains: boundary conditions permitting their formation and exhumation. PhD Thesis:University of Basel, pp 1-123.
    Bader, T., Franz, L., Ratschbacher, L., Capitani, C., Webb, A. A. G, Yang, Z., Pfander, J. A., Hofmann, M., Linnemann, U.2013b. The Heart of China revisited:Ⅱ Early Paleozoic (ultra) high-pressure and (ultra) high-temperature metamorphic Qinling orogenic collage. Tectonics,32(4):922-947.
    Bader, T., Ratschbacher, L., Franz, L., Yang, Z., Hofmann, M., Linnemann, U., Yuan, H.2013a. The Heart of China revisited, I. Proterozoic tectonics of the Qin Mountains in the core of supercontinent Rodinia.Tectonics,32(3):661-687.
    Bao, Z. W., Wang, Q., Bai, G D., Zhao, Z. H., Song, Y. W., Liu, X. M.2008. Geochronology and geochemistry of the Fangcheng Neoproterozoic alkali-syenites in East Qinling orogen and its geodynamic implications. Chinese Science Bulletin,53(13):2050-2061.
    Barbarin, B.1990. Granitoids:Main petrogenetic classifications in relation to origin and tectonic setting. Geological Journal,25(3-4):227-238.
    Bhatia, M. R.1983. Plate tectonics and geochemical composition of sandstones. The Journal of Geology,91(6):611-627.
    Black, L. P., Kamo, S. L., Allen, C. M., Davis, D. W., Aleinikoff, J. N., Valley, J. W., Mundil, R., Campbell, I. H., Korsch, R. J., Williams, I. S., Foudoulis, C.2004. Improved 206Pb/238U microprobe geochronology by the monitoring of a trace-element-related matrix effect; SHRIMP, ID-TIMS, ELA-ICP-MS and oxygen isotope documentation for a series of zircon standards. Chemical Geology,205(1-2):115-140.
    Blichert-Toft, J., Albarede, F.1997. The Lu-Hf isotope geochemistry of chondrites and the evolution of the mantle-crust system. Earth and Planetary Science Letters,148(1):243-258.
    Blichert-Toft, J., Albarede, F.2008. Hafnium isotopes in Jack Hills zircons and the formation of the Hadean crust. Earth and Planetary Science Letters,265(3-4):686-702.
    Boger, S. D., Carsonb, C. J., Wilsona, C. J. L., Fanning, C. M.2000. Neoproterozoic deformation in the Radok Lake region of the northern Prince Charles Mountains, east Antarctica; evidence for a single protracted orogenic event. Precambrian Research,104(1-2):1-24.
    Bonin, B., Azzouni-Sekkal, A., Bussy, F., Ferrag, S.1998. Alkali-calcic and alkaline post-orogenic (PO) granite magmatism:petrologic constraints and geodynamic settings. Lithos,45(1-4): 45-70.
    Brouxel, M., Lapierre, H., Michard, A., Albarede, F.1987. The deep layers of a Paleozoic arc: geochemistry of the Copley-Balaklala series, northern California. Earth and Planetary Science Letters,85(4):386-400.
    Brueckner, H. K.2009. Subduction of continental crust, the origin of post-orogenic granitoids (and anorthosites?) and the evolution of Fennoscandia. Journal of the Geological Society, 166(4):753-762.
    Chen, D. L., Liu, L., Sun, Y, Zhang, A. D., Liu, X. M., Luo, J. H.2004b. LA-ICP-MS zircon U-Pb dating for high-pressure basic granulite from North Qinling and its geological significance. Chinese Science Bulletin,49(21):2296-2304.
    Chen, D. L., Liu, L., Sun, Y, Zhang, A., Zhang, C. L., Liu, X. M., Luo, J. H.2004a. Determination of the neoproterozoic shicaogou syn-collisional granite in the eastern Qinling Mountains and its geological implications. Acta Geologica Sinica-English Edition,78(1):73-82.
    Chen, F., Hegner, E., Todt, W.2000. Zircon ages and Nd isotopic and chemical compositions of orthogneisses from the Black Forest, Germany:evidence for a Cambrian magmatic arc. International Journal of Earth Sciences,88(4):791-802.
    Chen, F., Li, X. H., Wang, X. L., Li, Q. L., Siebel, W.2007. Zircon age and Nd-Hf isotopic composition of the Yunnan Tethyan belt, southwestern China. International Journal of Earth Sciences,96(6):1179-1194
    Chen, F., Siebel, W., Satir, M., Terzioglu, M. N., Saka, K.2002. Geochronology of the Karadere basement (NW Turkey) and implications for the geological evolution of the Istanbul zone. International Journal of Earth Sciences,91(3):469-481.
    Chen, Z. H., Lu, S. N., Li, H. K., Li, H. M., Xiang, Z. Q., Zhou, H. Y, Song, B.2006. Constraining the role of the Qinling orogen in the assembly and break-up of Rodinia: Tectonic implications for Neoproterozoic granite occurrences. Journal of Asian Earth Sciences,28(1):99-115.
    Cheng, H., Zhang, C., Vervoort, J. D., Li, X. H., Li, Q. L., Zheng, S., Cao, D. D.2011. Geochronology of the transition of eclogite to amphibolite facies metamorphism in the North Qinling orogen of central China. Lithos,125(3-4):969-983.
    Cheng, H., Zhang, C., Vervoort, J. D., Li, X., Li, Q., Wu, Y, Zheng, S.2012. Timing of eclogite facies metamorphism in the North Qinling by U-Pb and Lu-Hf geochronology. Lithos, 136-139:46-59.
    Chu, N.-C., Taylor, R. N., Chavagnac, V., Nesbitt, R. W., Boella, R. M., Milton, J. A., German, C. R., Bayon, G, Burton, K.2002. Hf isotope ratio analysis using multi-collector inductively coupled plasma mass spectrometry:an evaluation of isobaric interference corrections. Journal of Analytical Atomic Spectrometry,17(12):1567-1574.
    Clemens, J. D., Stevens, G. 2012. What controls chemical variation in granitic magmas? Lithos, 134-135:317-329.
    Coleman, D. S., Glazner, A. F., Frost, T. P.1992. Evidence from the Lamarck Granodiorite for Rapid Late Cretaceous Crust Formation in California. Science,258(5090):1924-1926.
    Coulon, C., Maluski, H., Bollinger, C., Wang, S. K.1986. Mesozoic and cenozoic volcanic rocks from central and southern Tibet:39Ar-40Ar dating, petrological characteristics and geodynamical significance. Earth and Planetary Science Letters,79(3-4):281-302.
    Cui, M., Zhang, B., Zhang, L.2011. U-Pb dating of baddeleyite and zircon from the Shizhaigou diorite in the southern margin of North China Craton:Constrains on the timing and tectonic setting of the Paleoproterozoic Xiong'er group. Gondwana Research,20(1):184-193.
    Defant, M. J., Drummond, M. S.1990. Derivation of some modern arc magmas by melting of young subducted lithosphere. Nature,347(6294):662-665.
    Deng, Q., Wang, J., Wang, Z.-J., Wang, X.-C., Qiu, Y.-S., Yang, Q.-X., Du, Q.-D., Cui, X.-Z., Zhou, X.-L.2013. Continental flood basalts of the Huashan Group, northern margin of the Yangtze block-implications for the breakup of Rodinia. International Geology Review, 55(15):1865-1884.
    DePaolo, D. J.1988. Age dependence of the composition of continental crust:evidence from Nd isotopic variations in granitic rocks. Earth and Planetary Science Letters,90(3):263-271.
    DePaolo, D. J., Linn, A. M., Schubert, G. 1991. The continental crustal age distribution:Methods of determining mantle separation ages from Sm-Nd isotopic data and application to the southwestern United States. Journal of Geophysical Research:Solid Earth,96(B2): 2071-2088.
    Diwu, C. R., Sun, Y, Yan, Z., Liu, B. X., Lai, S. C.2014. Geochronological, geochemical and Nd-Hf isotopic studies of the Qingling Complex in the eastern Qinling, central China: implications for evolutionary history of the North Qinling Orogenic Belt prior to the Paleozoic. Geoscience Frontiers, Under review.
    Diwu, C. R., Sun, Y., Zhang, H., Wang, Q., Guo, A. L., Fan, L. G 2012. Episodic tectonothermal events of the western North China Craton and North Qinling Orogenic Belt in central China: Constraints from detrital zircon U-Pb ages. Journal of Asian Earth Sciences,47:107-122.
    Diwu, C., Sun, Y., Gao, J., Fan, L.2013. Early Precambrian tectonothermal events of the North China Craton:Constraints from in situ detrital zircon U-Pb, Hf and O isotopic compositions in Tietonggou Formation. Chinese Science Bulletin,58(31):3760-3770.
    Diwu, C., Sun, Y, Guo, A., Wang, H., Liu, X.2011. Crustal growth in the North China Craton at-2.5 Ga:Evidence from in situ zircon U-Pb ages, Hf isotopes and whole-rock geochemistry of the Dengfeng complex. Gondwana Research,20(1):149-170.
    Diwu, C., Sun, Y, Lin, C., Wang, H.2010. LA-(MC)-ICPMS U-Pb zircon geochronology and Lu-Hf isotope compositions of the Taihua complex on the southern margin of the North China Craton. Chinese Science Bulletin,55(23):2557-2571.
    Dong, Y P., Genser, J., Neubauer, F., Zhang, G W., Liu, X. M., Yang, Z., Heberer, B.2011a. U-Pb and 40Ar/39Ar geochronological constraints on the exhumation history of the North Qinling terrane, China Gondwana Research,19(4):881-893.
    Dong, Y. P., Liu, X. M., Neubauer, F., Zhang, G W, Tao, N., Zhang, Y. G, Zhang, X. N., Li, W. 2013. Timing of Paleozoic amalgamation between the North China and South China Blocks: Evidence from detrital zircon U-Pb ages. Tectonophysics,586:173-191.
    Dong, Y. P., Zhang, G W., Hauzenberger, C., Neubauer, F., Yang, Z., Liu, X. M.2011b. Palaeozoic tectonics and evolutionary history of the Qinling orogen:Evidence from geochemistry and geochronology of ophiolite and related volcanic rocks. Lithos,122(1-2):39-56.
    Dong, Y. P., Zhang, G W., Neubauer, F., Liu, X. M., Genser, J., Hauzenberger, C.2011c. Tectonic evolution of the Qinling orogen, China:Review and synthesis. Journal of Asian Earth Sciences,41(3):213-237.
    Dong, Y. P., Zhou, M. F., Zhang, G W., Zhou, D. W., Liu, L., Zhang, Q.2008. The Grenvillian Songshugou ophiolite in the Qinling Mountains, Central China:Implications for the tectonic evolution of the Qinling orogenic belt. Journal of Asian Earth Sciences,32(5-6):325-335.
    Duncan, A. R., Erlank, A. J., Marsh, J. S.1984. Regional geochemistry of the Karoo igneous province. Special Publication of Geological Society of South Africa,13:355-388.
    Elhlou, S., Belousova, E., Griffin, W., Pearson, N., O'reilly, S.2006. Trace element and isotopic composition of GJ-red zircon standard by laser ablation. Geochimica et Cosmochimica Acta, 70(18):A158.
    Enami, M., Qijia, Z.1990. Quartz pseudomorphs after coesite in eclogites from Shandong Province, East China. American Mineralogist,75(3-4):381-386.
    Gao, S., Ling, W., Qiu, Y., Lian, Z., Hartmann, G, Simon, K.1999. Contrasting geochemical and Sm-Nd isotopic compositions of Archean metasediments from the Kongling high-grade terrain of the Yangtze craton:evidence for cratonic evolution and redistribution of REE during crustal anatexis. Geochimica Et Cosmochimica Acta,63(13-14):2071-2088.
    Gao, S., Yang, J., Zhou, L., Li, M., Hu, Z., Guo, J., Yuan, H., Gong, H., Xiao, G., Wei, J.2011. Age and growth of the Archean Kongling terrain, South China, with emphasis on 3.3 Ga granitoid gneisses. American Journal of Science,311(2):153-182.
    Gao, S., Zhang, B. R., Wang, D. P., Ouyang, J. P., Xie, Q. L.1996. Geochemical evidence for the Proterozoic tectonic evolution of the Qinling orogenic belt and its adjacent margins of the north China and Yangtze cratons. Precambrian Research,80(1-2):23-48.
    Gao, S., Zhang, B. R., Xie, Q. L., Guo, X. M.1991. Proterozoic Intracontinental Rifting of the Qinling Orogenic Belt-Evidence from the Geochemistry of Sedimentary-Rocks. Chinese Science Bulletin,36(11):920-923.
    Gao, S., Zhang, B.-R., Gu, X.-M., Xie, Q.-L., Gao, C.-L., and Guo, X.-M.1995. Silurian-Devonian provenance changes of South Qinling basins:implications for accretion of the Yangtze (South China) to the North China cratons. Tectonophysics,250(1-3):183-197.
    Garland, F., Hawkesworth, C. J., Mantovani, M. S. M.1995. Description and Petrogenesis of the Parana Rzhyolites, Southern Brazil. Journal of Petrology,36(5):1193-1227.
    Geist, D., Howard, K., Larson, P.1995. The Generation of Oceanic Rhyolites by Crystal Fractionation:the Basalt-Rhyolite Association at Volcan Alcedo, Galapagos Archipelago. Journal of Petrology,36(4):965-982.
    Geng, Y., Du, L., Ren, L.2012. Growth and reworking of the early Precambrian continental crust in the North China Craton:Constraints from zircon Hf isotopes. Gondwana Research,21(2-3): 517-529.
    Greentree, M. R., Li, Z.-X.2008. The oldest known rocks in south-western China:SHRIMP U-Pb magmatic crystallisation age and detrital provenance analysis of the Paleoproterozoic Dahongshan Group. Journal of Asian Earth Sciences,33(5-6):289-302.
    Greentree, M. R., Li, Z.-X., Li, X.-H., Wu, H.2006. Late Mesoproterozoic to earliest Neoproterozoic basin record of the Sibao orogenesis in western South China and relationship to the assembly of Rodinia. Precambrian Research,151(1-2):79-100.
    Griffin, W. L., Pearson, N. J., Belousova, E., Jackson, S. E., van Achterbergh, E., O'Reilly, S. Y, Shee, S. R.2000. The Hf isotope composition of cratonic mantle:LAM-MC-ICPMS analysis of zircon megacrysts in kimberlites. Geochimica Et Cosmochimica Acta,64(1):133-147.
    Griffin, W. L., Wang, X., Jackson, S. E., Pearson, N. J., O'Reilly, S. Y, Xu, X. S., Zhou, X. M. 2002. Zircon chemistry and magma mixing, SE China:In-situ analysis of Hf isotopes, Tonglu and Pingtan igneous complexes. Lithos,61(3-4):237-269.
    Hacker, B. R., Ratschbacher, L., Liou, J. G 2004. Subduction, collision and exhumation in the ultrahigh-pressure Qinling-Dabie orogen. Aspects of the Tectonic Evolution of China, Geologica Society, London, Special Publication,226(1):157-175.
    Harrison, T. M., Blichert-Toft, J., Miiller, W., Albarede, F., Holden, P., Mojzsis, S. J.2005. Heterogeneous Hadean Hafnium:Evidence of Continental Crust at 4.4 to 4.5 Ga. Science, 310(5756):1947-1950.
    Hawkesworth, C. J., Dhuime, B., Pietranik, A. B., Cawood, P. A., Kemp, A. I. S., Storey, C. D. 2010. The generation and evolution of the continental crust. Journal of the Geological Society, 167(2):229-248.
    Hawkesworth, C. J., Kemp, A. I. S.2006a. Evolution of the continental crust. Nature,443(7113): 811-817.
    Hawkesworth, C. J., Kemp, A. I. S.2006b. Using hafnium and oxygen isotopes in zircons to unravel the record of crustal evolution. Chemical Geology,226(3-4):144-162.
    He, Y., Li, S., Hoefs, J., Huang, F., Liu, S.-A., Hou, Z.2011. Post-collisional granitoids from the Dabie orogen:New evidence for partial melting of a thickened continental crust. Geochimica Et Cosmochimica Acta,75(13):3815-3838.
    He, Y, Zhao, G, Sun, M.2010. Geochemical and Isotopic Study of the Xiong'er Volcanic Rocks at the Southern Margin of the North China Craton. Petrogenesis and Tectonic Implications. The Journal of Geology,118(4):417-433.
    He, Y, Zhao, G, Sun, M., Wilde, S. A.2008. Geochemistry, isotope systematics and petrogenesis of the volcanic rocks in the Zhongtiao Mountain:An alternative interpretation for the evolution of the southern margin of the North China Craton. Lithos,102(1-2):158-178.
    He, Y, Zhao, G, Sun, M., Xia, X.2009. SHRIMP and LA-ICP-MS zircon geochronology of the Xiong'er volcanic rocks:Implications for the Paleo-Mesoproterozoic evolution of the southern margin of the North China Craton. Precambrian Research,168(3-4):213-222.
    Hochstaedter, A. G, Gill, J. B., Morris, J. D.1990. Volcanism in the Sumisu Rift, II. Subduction and non-subduction related components. Earth and Planetary Science Letters,100(1-3): 195-209.
    Hsu, K. J., Wang, Q. C., Li, J. L., Zhou, D., Sun, S.1987. Tectonic Evolution of Qinling Mountains, China. Eclogae Geologicae Helvetiae,80(3):735-752.
    Hu, J., Liu, X., Chen, L., Qu, W., Li, H., and Geng, J.2013. A ~2.5 Ga magmatic event at the northern margin of the Yangtze craton:Evidence from U-Pb dating and Hf isotope analysis of zircons from the Douling Complex in the South Qinling orogen. Chinese Science Bulletin, 58(28-29):3564-3579.
    Hu, N. G, Yang, J. X., An, S. Y., Hu, J. M.1993. Metamorphism and tectonic evolution of the Shangdan fault zone, Shaanxi, China. Journal of Metamorphic Geology,11(4):537-548.
    Hu, N. G, Zhao, D. G, Xu, B. Q., Wang, T.1995. Discovery of Coesite-Bearing Eclogites from the Northern Qinling and Its Significances. Chinese Science Bulletin,40(2):174-176.
    Huang, W., Wu, Z. W.1992. Evolution of the Qinling Orogenic Belt. Tectonics,11(2):371-380.
    Huang, X.-L., Niu, Y, Xu, Y.-G, Yang, Q.-J., and Zhong, J.-W..2010. Geochemistry of TTG and TTG-like gneisses from Lushan-Taihua complex in the southern North China Craton: Implications for late Archean crustal accretion. Precambrian Research,182(1-2):43-56.
    Irvine, T. N., Baragar, W. R. A.1971. A guide to the chemical classification of the common volcanic rocks. Canadian Journal of Earth Sciences,8(5):523-548.
    Jahn, B.-m., Liu, D., Wan, Y, Song, B., Wu, J.2008. Archean crustal evolution of the Jiaodong Peninsula, China, as revealed by zircon SHRIMP geochronology, elemental and Nd-isotope geochemistry. American Journal of Science,308(3):232-269.
    Jahn, B.-m., Wu, F., Chen, B.2000. Granitoids of the Central Asian Orogenic Belt and continental growth in the Phanerozoic. Transactions of the Royal Society of Edinburgh:Earth Sciences, 91(1-2):181-193.
    Jahn, B.-m., Wu, F., Lo, C.-H., Tsai, C.-H.1999. Crust-mantle interaction induced by deep subduction of the continental crust:geochemical and Sr-Nd isotopic evidence from post-collisional mafic-ultramafic intrusions of the northern Dabie complex, central China. Chemical Geology,157(1-2):119-146.
    Jiang, N., Carlson, R. W., Guo, J.2011. Source of Mesozoic intermediate-felsic igneous rocks in the North China craton:Granulite xenolith evidence. Lithos,125(1-2):335-346.
    Jiang, N., Guo, J., Zhai, M., Zhang, S.2010a.-2.7 Ga crust growth in the North China craton. Precambrian Research,179(1-4):37-49.
    Jiang, Y. H., Jin, G D., Liao, S. Y, Zhou, Q., Zhao, P.2010b. Geochemical and Sr-Nd-Hf isotopic constraints on the origin of Late Triassic granitoids from the Qinling orogen, central China: Implications for a continental arc to continent-continent collision. Lithos,117(1-4):183-197.
    Jiao, W., Wu, Y, Yang, S., Peng, M., Wang, J.2009. The oldest basement rock in the Yangtze Craton revealed by zircon U-Pb age and Hf isotope composition. Science in China Series D: Earth Sciences,52(9):1393-1399.
    Kemp, A. I. S., Hawkesworth, C. J.2003. Granitic perspectives on the generation and secular evolution of the continental crust, In:Rudnick, R. L., ed., Treatise on Geochemistry, Volume 3:The Crust, Elsevier-Pergamon, Oxford, pp 349-410.
    Kemp, A. I. S., Hawkesworth, C. J., Foster, G L., Paterson, B. A., Woodhead, J. D., Hergt, J. M., Gray, C. M., Whitehouse, M. J.2007. Magmatic and Crustal Differentiation History of Granitic Rocks from Hf-O Isotopes in Zircon. Science,315(5814):980-983.
    Kemp, A. I. S., Hawkesworth, C. J., Paterson, B. A., Kinny, P. D.2006. Episodic growth of the Gondwana supercontinent from hafnium and oxygen isotopes in zircon. Nature,439(7076): 580-583.
    Kroner, A., Compston, W., Guo-wei, Z., An-lin, G., Todt, W.1988. Age and tectonic setting of Late Archean greenstone-gneiss terrain in Henan Province, China, as revealed by single-grain zircon dating. Geology,16(3):211-215.
    Kroner, A., Zhang, G W., Sun, Y.1993. Granulites in the Tongbai Area, Qinling Belt, China-Geochemistry, Petrology, Single Zircon Geochronology, and Implications for the Tectonic Evolution of Eastern Asia. Tectonics,12(1):245-255.
    Kustera, D., Harmsb, U.1998. Post-collisional potassic granitoids from the southern and northwestern parts of the Late Neoproterozoic East African Orogen:a review. Lithos,45(1-4): 177-195.
    Lai, S. C., Zhang, G W., Li, S. Z.2004. Ophiolites from the Mianlue Suture in the Southern Qinling and Their Relationship with the Eastern Paleotethys Evolution. Acta Geologica Sinica-English Edition,78(1):107-117.
    Lai, S., Qin, J., Chen, L., Grapes, R..2008. Geochemistry of ophiolites from the Mian-Lue Suture Zone:implications for the tectonic evolution of the Qinling Orogen, Central China. International Geology Review,50(7):650-664.
    Le Maitre, R. W., Bateman, P., Dudek, A., Keller, J., Lameyre, M., Lebas, M. J., Sabine, P. A., Schmid, R., Sorensen, H., Streckeisen, A., Woolley, A. R., Zanettin, B.1989. A Classification of Igneous Rocks and a Glossary of Terms. Blackwell Scientific Publications, Oxford, pp 1-193.
    Li, L.-M., Sun, M., Wang, Y, Xing, G, Zhao, G, He, Y, He, K., Zhang, A.2011. U-Pb and Hf isotopic study of detrital zircons from the meta-sedimentary rocks in central Jiangxi Province, South China:Implications for the Neoproterozoic tectonic evolution of South China Block. Journal of Asian Earth Sciences,41(1):44-55.
    Li, Q.-L., Li, X.-H., Liu, Y, Tang, G.-Q., Yang, J.-H., Zhu, W.-G. 2010. Precise U-Pb and Pb-Pb dating of Phanerozoic baddeleyite by SIMS with oxygen flooding technique. Journal of Analytical Atomic Spectrometry,25(7):1107-1113.
    Li, S. G., Hart, S. R., Guo, A. L., Zhang, G. W.1988. Sm-Nd WHOLE-ROCK ISOCHRON AGE OF THE DENGFENG GROUP IN CENTRAL HENAN AND ITS TECTONIC IMPLICATION. Chinese Science Bulletin,33(20):1714-1717.
    Li, S. Z., Kusky, T. M., Wang, L., Zhang, G W., Lai, S. C., Liu, X. C., Dong, S. W., Zhao, G C. 2007. Collision leading to multiple-stage large-scale extrusion in the Qinling orogen:insights from the Mianlue suture. Gondwana Research,12(1):121-143
    Li, X. H., Li, W. X., Li, Q. L., Wang, X. C., Liu, Y., Yang, Y. H.2010. Petrogenesis and tectonic significance of the ~850 Ma Gangbian alkaline complex in South China:Evidence from in situ zircon U-Pb dating, Hf-O isotopes and whole-rock geochemistry. Lithos,114(1-2):1-15
    Li, X., Li, W., Wang, X., Li, Q., Liu, Y., Tang, G 2009b. Role of mantle-derived magma in genesis of early Yanshanian granites in the Nanling Range, South China:in situ zircon Hf-O isotopic constraints. Science in China Series D:Earth Sciences,52(9):1262-1278.
    Li, X.-H., Liu, Y., Li, Q.-L., Guo, C.-H., Chamberlain, K. R.2009a. Precise determination of Phanerozoic zircon Pb/Pb age by multicollector SIMS without external standardization. Geochemistry, Geophysics, Geosystems,10, Q04010, doi:10.1029/2009GC002400.
    Li, Y, Lai, S., Qin, J., Liu, X., Wang, J.2007. Geochemical characteristics of Bikou volcanic group and Sr-Nd-Pb isotopic composition:Evidence for breakup event in the north margin of Yangtze plate, Jining era. Science in China Series D:Earth Sciences,50(2):339-350.
    Li, Z. X., Li, X. H., Kinny, P. D., Wang, J.1999. The breakup of Rodinia:did it start with a mantle plume beneath South China? Earth and Planetary Science Letters,173(3):171-181.
    Liegeois, J. P.1998. Some words on the post-collisional magmatism. Lithos,45:XV-XVII.
    Ling, W., Duan, R., Liu, X., Cheng, J., Mao, X., Peng, L., Liu, Z., Yang, H., Ren, B.2010. U-Pb dating of detrital zircons from the Wudangshan Group in the South Qinling and its geological significance. Chinese Science Bulletin,55(22):2440-2448.
    Ling, W., Gao, S., Zhang, B., Li, H., Liu, Y, Cheng, J.2003. Neoproterozoic tectonic evolution of the northwestern Yangtze craton, South China:implications for amalgamation and break-up of the Rodinia Supercontinent. Precambrian Research,122(1-4):111-140.
    Ling, W., Ren, B., Duan, R., Liu, X., Mao, X., Peng, L., Liu, Z., Cheng, J., Yang, H.2008. Timing of the Wudangshan, Yaolinghe volcanic sequences and mafic sills in South Qinling:U-Pb zircon geochronology and tectonic implication. Chinese Science Bulletin,53(14):2192-2199.
    Liu, B.-X., Qi, Y, Wang, W., Siebel, W., Zhu, X.-Y, Nie, H., He, J.-F., Chen, F. K.2013a. Zircon U-Pb ages and O-Nd isotopic composition of basement rocks in the North Qinling Terrain, central China:evidence for provenance and evolution. International Journal of Earth Sciences, 102:2153-2173.
    Liu, C., Zhao, G., Sun, M., Zhang, J., Yin, C., He, Y.2012. Detrital zircon U-Pb dating, Hf isotopes and whole-rock geochemistry from the Songshan Group in the Dengfeng Complex: Constraints on the tectonic evolution of the Trans-North China Orogen. Precambrian Research,192-195:1-15.
    Liu, D., Wilde, S. A., Wan, Y, Wang, S., Valley, J. W., Kita, N., Dong, C., Xie, H., Yang, C., Zhang, Y, Gao, L.2009a. Combined U-Pb, hafnium and oxygen isotope analysis of zircons from meta-igneous rocks in the southern North China Craton reveal multiple events in the Late Mesoarchean-Early Neoarchean. Chemical Geology,261(1-2):140-154.
    Liu, F., Guo, J., Lu, X., Diwu, C.2009b. Crustal growth at ~2.5 Ga in the North China Craton: evidence from whole-rock Nd and zircon Hf isotopes in the Huai'an gneiss terrane. Chinese Science Bulletin,54(24):4704-4713.
    Liu, L., Chen, D. L., Zhang, A. D., Zhang, C. L., Yuan, H. L., Luo, J. H.2004b. Geochemical Characteristics and LA-ICP-MS Zircon U-Pb Dating of Amphibolites in the Songshugou Ophiolite in the Eastern Qinling. Acta Geologica Sinica-English Edition,78(1):137-145.
    Liu, L., Sun, Y, Luo, J. H., Wang, Y, Chen, D. L., Zhang, A. D.2004a. Ultra-high pressure metamorphism of granitic gneiss in the Yinggelisayi area, Altun Mountains, NW China. Science in China Series D:Earth Sciences,47(4):338-346.
    Liu, L., Yang, J., Chen, D., Wang, C., Zhang, C., Yang, W., Cao, Y 2010. Progress and controversy in the study of HP-UHP metamorphic terranes in the West and Middle Central China orogen. Journal of Earth Science,21(5):581-597.
    Liu, L., Zhou, D. W.1995. Discovery and Study of High-Pressure Basic Granulites in Songshugou Area of Shangnan, East Qinling. Chinese Science Bulletin,40(5):400-404.
    Liu, L., Zhou, D. W., Wang, Y, Chen, D. L.1996. Study and implication of the high-pressure felsic granulite in the Qinling complex of east Qinling. Science in China (Series D), 26(Suppl):60-68.
    Liu, Q., Wu, Y B., Wang, H., Gao, S., Qin, Z. W., Liu, X. C., Yang, S. H., Gong, H. J.2013c. Zircon U-Pb ages and Hf isotope compositions of migmatites from the North Qinling terrane and their geological implications. Journal of Metamorphic Geology,.
    Liu, R., Li, J.-W, Bi, S.-J., Hu, H., Chen, M.2013b. Magma mixing revealed from in situ zircon U-Pb-Hf isotope analysis of the Muhuguan granitoid pluton, eastern Qinling Orogen, China: implications for late Mesozoic tectonic evolution. International Journal of Earth Sciences, 102(6):1583-1602.
    Liu, S.-A., Li, S., He, Y, Huang, F. 2010. Geochemical contrasts between early Cretaceous ore-bearing and ore-barren high-Mg adakites in central-eastern China:implications for petrogenesis and Cu-Au mineralization. Geochimica Et Cosmochimica Acta,74(24): 7160-7178.
    Liu, X. M., Gao, S., Diwu, C. R., Yuan, H. L., Hu, Z. C.2007. Simultaneous in-situ determination of U-Pb age and trace elements in zircon by LA-ICP-MS in 20 μm spot size. Chinese Science Bulletin,52(9):1257-1264.
    Liu, X., Gao, S., Diwu, C., Ling, W.2008. Precambrian crustal growth of Yangtze Craton as revealed by detrital zircon studies. American Journal of Science,308(4):421-468.
    Liu, Y, Gao, S., Yuan, H., Zhou, L., Liu, X., Wang, X., Hu, Z., Wang, L.2004c. U-Pb zircon ages and Nd, Sr, and Pb isotopes of lower crustal xenoliths from North China Craton:insights on evolution of lower continental crust. Chemical Geology,211(1-2):87-109.
    Lu, S., Yang, C., Li, H., Li, H.2002. A Group of Rifting Events in the Terminal Paleoproterozoic in the North China Craton. Gondwana Research,5(1):123-131.
    Ludwig, K. R.2003. ISOPLOT 3.00:A Geochronological Toolkit for Microsoft Excel. Berkeley Geochronology Center, Special Publication, California, Berkeley.
    Mao, J. W., Xie, G. Q., Pirajno, F., Ye, H. S., Wang, Y. B., Li, Y. F., Xiang, J. F., Zhao, H. J.2010. Late Jurassic-Early Cretaceous granitoid magmatism in Eastern Qinling, central-eastern China:SHRIMP zircon U-Pb ages and tectonic implications. Australian Journal of Earth Sciences,57(1):51-78.
    Mattauer, M., Matte, P., Malavieille, J., Tapponnier, P., Maluski, H., Xu, Z. Q., Lu, Y. L., Tang, Y. Q.1985. Tectonics of the Qinling Belt-Buildup and Evolution of Eastern Asia. Nature, 317(6037):496-500.
    McCulloch, M., Wasserburg, G.1978. Sm-Nd and Rb-Sr chronology of continental crust formation. Science,200(4345):1003-1011.
    Meng, Q. R., Zhang, G W.1999. Timing of collision of the North and South China blocks: Controversy and reconciliation. Geology,27(2):123-126.
    Meng, Q. R., Zhang, G W.2000. Geologic framework and tectonic evolution of the Qinling orogen, central China. Tectonophysics,323(3-4):183-196.
    Nelson, B. K., DePAOLO, D. J.1985. Rapid production of continental crust 1.7 to 1.9 by ago:Nd isotopic evidence from the basement of the North American mid-continent. Geological Society of America Bulletin,96(6):746-754.
    Nowell, G, Kempton, P., Noble, S., Fitton, J., Saunders, A., Mahoney, J., Taylor, R.1998. High precision Hf isotope measurements of MORB and OIB by thermal ionisation mass spectrometry:insights into the depleted mantle. Chemical Geology,149(3):211-233.
    Okay, A. I., Xu, S. T., Sengor A. M. C.1989. Coesite from the Dabie Shan eclogites, central China. European Journal of Mineralogy,1(4):595-598.
    Page, F. Z., Fu, B., Kita, N. T., Fournelle, J., Spicuzza, M. J., Schulze, D. J., Viljoen, F., Basei, M. A. S., Valley, J. W.2007. Zircons from kimberlite:New insights from oxygen isotopes, trace elements, and Ti in zircon thermometry. Geochimica Et Cosmochimica Acta,71(15): 3887-3903.
    Pearce, J. A.1976. Statistical Analysis of Major Element Patterns in Basalts. Journal of Petrology, 17:15-43.
    Pearce, J. A.1983. Role of the sub-continental lithosphere in magma genesis at active continental margins. In:Hawkesworth C. J. and Norry M. J. (eds.), Continental basalts and mantle xenoliths, Nantwich:Shiva, pp 230-249.
    Pearce, J. A., Harris, N. B. W., Tindle, A. G 1984. Trace Element Discrimination Diagrams for the Tectonic Interpretation of Granitic Rocks. Journal of Petrology,25(4):956-983.
    Peng, M., Wu, Y., Gao, S., Zhang, H., Wang, J., Liu, X., Gong, H., Zhou, L., Hu, Z., Liu, Y., Yuan, H.2012. Geochemistry, zircon U-Pb age and Hf isotope compositions of Paleoproterozoic aluminous A-type granites from the Kongling terrain, Yangtze Block:Constraints on petrogenesis and geologic implications. Gondwana Research,22(1):140-151.
    Peng, P., Zhai, M., Ernst, R. E., Guo, J., Liu, F., Hu, B.2008. A 1.78 Ga large igneous province in the North China craton:The Xiong'er Volcanic Province and the North China dyke swarm. Lithos,101(3-4):260-280.
    Pin, C., Marin, F.1993. Early Ordovician continental break-up in Variscan Europe:Nd-Sr isotope and trace element evidence from bimodal igneous associations of the Southern Massif Central, France. Lithos,29(3-4):177-196.
    Ping, X., Zheng, J., Zhao, J., Tang, H., Griffin, W. L.2013. Heterogeneous sources of the Triassic granitoid plutons in the southern Qinling orogen:An E-W tectonic division in central China. Tectonics,32(3):396-416.
    Qin, J. F., Lai, S. C., Grapes, R., Diwu, C. R., Ju, Y. J., Li, Y. F.2009. Geochemical evidence for origin of magma mixing for the Triassic monzonitic granite and its enclaves at Mishuling in the Qinling orogen (central China). Lithos,112(3-4):259-276.
    Qin, J. F., Lai, S. C., Grapes, R., Diwu, C. R., Ju, Y. J., Li, Y. F.2010. Origin of LateTriassic high-Mg adakitic granitoid rocks from the Dongjiangkou area, Qinling orogen, central China Implications for subduction of continental crust. Lithos,120(3-4):347-367.
    Qin, J. F., Lai, S. C., Li, Y. F.2008a. Slab Breakoff Model for the Triassic Post-Collisional Adakitic Granitoids in the Qinling Orogen, Central China:Zircon U-Pb Ages, Geochemistry, and Sr-Nd-Pb Isotopic Constraints. International Geology Review,50(12):1080-1104.
    Qin, J. F., Lai, S. C., Wang, J., Li, Y. F.2007. High-Mg# adakitic tonalite from the xichahe area, South Qinling orogenic belt (Central China):Petrogenesis and geological implications. International Geology Review,49(12):1145-1158.
    Qin, J. F., Lai, S. C., Wang, J., Li, Y. F. 2008b. Zircon LA-ICP MS U-Pb age, Sr-Nd-Pb isotopic compositions and geochemistry of the Triassic post-collisional Wulong adakitic granodiorite in the South Qinling, Central China, and its petrogenesis. Acta Geologica Sinica-English Edition,82(2):425-437.
    Qiu, Y. M., Gao, S., McNaughton, N. J., Groves, D. I., Ling, W.2000. First evidence of>3.2 Ga continental crust in the Yangtze craton of south China and its implications for Archean crustal evolution and Phanerozoic tectonics. Geology,28(1):11-14.
    Ratschbacher, L., Hacker, B. R., Calvert, A., Webb, L. E., Grimmer, J. C, McWilliams, M. O., Ireland, T., Dong, S. W., Hu, J. M.2003. Tectonics of the Qinling (Central China): tectonostratigraphy, geochronology, and deformation history. Tectonophysics,366(1-2):1-53.
    Rickwood, P. C.1989. Boundary lines within petrologic diagrams which use oxides of major and minor elements. Lithos,22(4):247-263.
    Scherer, E., Munker, C., Mezger, K.2001. Calibration of the lutetium-hafnium clock. Science, 293(5530):683-687.
    Sengor, A. M. C.1985. Geology:East Asian tectonic collage. Nature,318(6041):16-17.
    Shi, Y, Yu, J.-H., Santosh, M.2013. Tectonic evolution of the Qinling orogenic belt, Central China:New evidence from geochemical, zircon U-Pb geochronology and Hf isotopes. Precambrian Research,231:19-60.
    Simonen, A.1953. Stratigraphy and sedimentation of the Svecofennidic, early Archean supracrustal rocks in southwestern Finland. Bulletin de la Commission geologique de Finlande,160:64.
    Song, S. G., Yang, J. S., Xu, Z. Q., Liou, J. G., Shi, R. D.2003a. Metamorphic evolution of the coesite-bearing ultrahigh-pressure terrane in the North Qaidam, Northern Tibet, NW China. Journal of Metamorphic Geology,21(6):631-644.
    Song, S., Yang, J., Liou, J. G., Wu, C., Shi, R., Xu, Z.2003b. Petrology, geochemistry and isotopic ages of eclogites from the Dulan UHPM Terrane, the North Qaidam, NW China. Lithos, 70(3-4):195-211.
    Song, S., Zhang, L., Niu, Y, Su, L., Jian, P., Liu, D.2005. Geochronology of diamond-bearing zircons from garnet peridotite in the North Qaidam UHPM belt, Northern Tibetan Plateau:A record of complex histories from oceanic lithosphere subduction to continental collision., Earth and Planetary Science Letters,234(1-2):99-118.
    Stacey, J. t., Kramers, J.1975. Approximation of terrestrial lead isotope evolution by a two-stage model. Earth and Planetary Science Letters,26(2):207-221.
    Sun, J.-F., Yang, J.-H., Wu, F.-Y., Wilde, S. A.2012. Precambrian crustal evolution of the eastern North China Craton as revealed by U-Pb ages and Hf isotopes of detrital zircons from the Proterozoic Jing'eryu Formation. Precambrian Research,200-203:184-208.
    Sun, S. S., McDonough, W.1989. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes. In:Saunders AD and Norry MJ (eds) Magmatism in the ocean basins. Special Publications, Geological Society, London,42(1): 313-345.
    Sun, W. D., Li, S. G, Chen, Y. D., Li, Y. J.2002a. Timing of synorogenic granitoids in the South Qinling, central China:Constraints on the evolution of the Qinling-Dabie orogenic belt; Journal of Geology,110(4):457-468.
    Sun, W. D., Li, S. G, Sun, Y., Zhang, G W., Li, Q. L.2002b. Mid-paleozoic collision in the north Qinling:Sm-Nd, Rb-Sr and 40Ar/39Ar ages and their tectonic implications. Journal of Asian Earth Sciences,21(1):69-76.
    Sun, Y., Lu, X. X., Han, S., Zhang, G. W.1996. Composition and formation of Palaeozoic Erlangping ophiolitic slab, North Qinling:Evidence from geology and geochemistry. Science in China (Series D),39 (suppl.):50-59.
    Tian, W., Wei, C. J.2005. The Caledonian low Al-TTD series from the Northern Qinling Orogenic Belt:Rock properties, genetic simulation and geological implication. Science in China Series D:Earth Sciences,48(11):1837-1847.
    Valley, J. W., Kinny, P. D., Schulze, D. J., Spicuzza, M. J.1998. Zircon megacrysts from kimberlite:oxygen isotope variability among mantle melts. Contributions to Mineralogy and Petrology,133(1-2):1-11.
    Wan, Y, Liu, D., Wang, S., Yang, E., Wang, W, Dong, C, Zhou, H., Du, L., Yang, Y, Diwu, C. 2011.-2.7 Ga juvenile crust formation in the North China Craton (Taishan-Xintai area, western Shandong Province):Further evidence of an understated event from U-Pb dating and Hf isotopic composition of zircon. Precambrian Research,186(1-4,):169-180.
    Wan, Y, Liu, D., Xu, M., Zhuang, J., Song, B., Shi, Y, Du, L.2007. SHRIMP U-Pb zircon geochronology and geochemistry of metavolcanic and metasedimentary rocks in Northwestern Fujian, Cathaysia block, China:Tectonic implications and the need to redefine lithostratigraphic units. Gondwana Research,12(1-2):166-183.
    Wan, Y, Wilde, S. A., Liu, D., Yang, C., Song, B., Yin, X.2006. Further evidence for ~1.85 Ga metamorphism in the Central Zone of the North China Craton:SHRIMP U-Pb dating of zircon from metamorphic rocks in the Lushan area, Henan Province. Gondwana Research, 9(1-2):189-197.
    Wang, C. Y., Campbell, I. H., Allen, C. M., Williams, I. S., Eggins, S. M.2009a. Rate of growth of the preserved North American continental crust:Evidence from Hf and O isotopes in Mississippi detrital zircons. Geochimica Et Cosmochimica Acta,73(3):712-728.
    Wang, F., Zhu, L. M., Li, J. M., Lee, B., Gong, H. J., Yang, T., Wang, W., Xu, A.2011a. Zircon U-Pb ages and Hf isotopic characteristics of the Dehe biotite monzonitic gneiss pluton in the North Qinling orogen and their geological significance. Chinese Journal of Geochemistry, 30(2):204-216.
    Wang, H., Wu, Y. B., Gao, S., Liu, X. C., Gong, H. J., Li, Q. L., Li, X. H., Yuan, H. L.2011b. Eclogite origin and timings in the North Qinling terrane, and their bearing on the amalgamation of the South and North China Blocks. Journal of Metamorphic Geology,29(9): 1019-1031.
    Wang, H., Wu, Y.-B., Gao, S., Liu, X.-C., Liu, Q., Qin, Z.-W, Xie, S.-W, Zhou, L., Yang, S.-H. 2013a. Continental origin of eclogites in the North Qinling terrane and its tectonic implications. Precambrian Research,230:13-30.
    Wang, H., Wu, Y.-B., Gao, S., Zheng, J.-P., Liu, Q., Liu, X.-C., Qin, Z.-W., Yang, S.-H., Gong, H.-J.2014. Deep subduction of continental crust in accretionary orogen:Evidence from U-Pb dating on diamond-bearing zircons from the Qinling orogen, central China. Lithos,190-191: 420-429.
    Wang, L.-J., Griffin, W. L., Yu, J.-H., O'Reilly, S. Y.2013b. U-Pb and Lu-Hf isotopes in detrital zircon from Neoproterozoic sedimentary rocks in the northern Yangtze Block:implications for Precambrian crustal evolution. Gondwana Research,23(4):1261-1272.
    Wang, Q.2005. Petrogenesis of Adakitic Porphyries in an Extensional Tectonic Setting, Dexing, South China. Implications for the Genesis of Porphyry Copper Mineralization:Journal of Petrology,47(1):119-144.
    Wang, T., Pei, X. Z., Wang, X. X., Hu, N. G, Li, W. P., Zhang, G W.2005. Orogen-parallel westward oblique uplift of the Qinling basement complex in the core of the Qinling orogen (China):An example of oblique extrusion of deep-seated metamorphic rocks in a collisional orogen. Journal of Geology,113(2):181-200.
    Wang, T., Wang, X. X., Tian, W, Zhang, C. L., Li, W. P., Li, S.2009b. North Qinling Paleozoic granite associations and their variation in space and time:Implications for orogenic processes in the orogens of central China. Science in China Series D:Earth Sciences,52(9):1359-1384.
    Wang, T., Wang, X. X., Zhang, G. W., Pei, X. Z., Zhang, C. L.2003. Remnants of a Neoproterozoic collisional orogenic belt in the core of the phanerozoic Qinling orogenic belt (China). Gondwana Research,6(4):699-710.
    Wang, W., Zhai, M., Wang, S., Santosh, M., Du, L., Xie, H., Lv, B., Wan, Y.2013c. Crustal reworking in the North China Craton at ~2.5 Ga:evidence from zircon U-Pb age, Hf isotope and whole rock geochemistry of the felsic volcano-sedimentary rocks from the western Shandong Province. Geological Journal,48(5):406-428.
    Wang, X. M., Liou, J. G, Mao, H. K.1989. Coesite-bearing eclogite from the Dabie Mountains in central China. Geology,17(12):1085-1088.
    Wang, X. X., Wang, T., Zhang, C. L.2013d. Neoproterozoic, Paleozoic, and Mesozoic granitoid magmatism in the Qinling Orogen, China:Constraints on orogenic process. Journal of Asian Earth Sciences,72:129-151.
    Wang, X.-L., Jiang, S.-Y, Dai, B.-Z.2010. Melting of enriched Archean subcontinental lithospheric mantle:Evidence from the ca.1760 Ma volcanic rocks of the Xiong'er Group, southern margin of the North China Craton. Precambrian Research,182(3):204-216.
    Wiedenbeck, M., A11E, P., Corfu, F., Griffin, W. L., Meier, M., Oberli, F., Quadt, A. V., Roddick, J. C, Spiegel, W.1995. THREE NATURAL ZIRCON STANDARDS FOR U-TH-PB, LU-HF, TRACE ELEMENT AND REE ANALYSES. Geostandards Newsletter,19(1):1-23.
    Wiedenbeck, M., Hanchar, J. M., Peck, W. H., Sylvester, P., Valley, J., Whitehouse, M., Kronz, A., Morishita, Y, Nasdala, L., Fiebig, J., Franchi, I., Girard, J.-P., Greenwood, R. C., Hinton, R., Kita, N., Mason, P. R. D., Norman, M., Ogasawara, M., Piccoli, P. M., Rhede, D., Satoh, H., Schulz-Dobrick, B., Skar,(?)., Spicuzza, M. J., Terada, K., Tindle, A., Togashi, S., Vennemann, T., Xie, Q., Zheng, Y.-F.2004. Further characterisation of the 91500 zircon crystal: Geostandards and Geoanalytical Research,28(1):9-39.
    Wong, W. H.1929. The Mesozoic Orogenic Movement in Eastern China. Bulletin of the Geological Society of China,8(1):33-44.
    Wu, F.-Y, Yang, Y.-H., Xie, L.-W., Yang, J.-H., Xu, P.2006. Hf isotopic compositions of the standard zircons and baddeleyites used in U-Pb geochronology. Chemical Geology,234(1-2): 105-126.
    Wu, H. Q., Feng, Y. M., Song, S. G.1993. Metamorphism and deformation of blueschist belts and their tectonic implications, North Qilian Mountains, China. Journal of Metamorphic Geology, 11(4):523-536.
    Wu, L., Jia, D., Li, H., Deng, F. E. I., Li, Y.2010. Provenance of detrital zircons from the late Neoproterozoic to Ordovician sandstones of South China:implications for its continental affinity. Geological Magazine,147(06):974-980.
    Wu, Y. B., Zheng, Y. F.2013. Tectonic evolution of a composite collision orogen:An overview on the Qinling-Tongbai-Hong'an-Dabie-Sulu orogenic belt in central China. Gondwana Research,23(4):1402-1428.
    Xia, L. Q., Xia, Z. C., Xu, X. Y.1996. Properties of middle-late Proterozoic volcanic rocks in South Qinling and the Precambrian continental break-up. Science in China (Series D),39(3): 256-265.
    Xia, X., Sun, M., Zhao, G., Luo, Y.2006a. LA-ICP-MS U-Pb geochronology of detrital zircons from the Jining Complex, North China Craton and its tectonic significance. Precambrian Research,144(3-4):199-212.
    Xia, X., Sun, M., Zhao, G., Wu, F., Xu, P., Zhang, J., Luo, Y.2006b. U-Pb and Hf isotopic study of detrital zircons from the Wulashan khondalites:Constraints on the evolution of the Ordos Terrane, Western Block of the North China Craton. Earth and Planetary Science Letters, 241(3-4):581-593.
    Xiong, Q., Zheng, J., Yu, C., Su, Y, Tang, H., Zhang, Z.2008. Zircon U-Pb age and Hf isotope of Quanyishang A-type granite in Yichang:signification for the Yangtze continental cratonization in Paleoproterozoic. Chinese Science Bulletin,54(3):436-446.
    Xu, J. F., Han, Y. W.1996. High radioactive Pb-isotope composition of ancient MORB-type rocks from Qinling area-Evidence for the presence of Tethyan-type oceanic mantle. Science in China (Series D),26(Suppl.):33-42
    Xu, J. F., Zhang, B. R., Han, Y. W.1996. Discovery of high radiogenic Pb isotopic composition from Pro-terozoic mafic rocks in North Qinling area and its implication. Chinese Science Bulletin,42(1):51-54
    Xu, J. F., Zhang, B. R., Han, Y. W.1997. Discovery of high radiogenic Pb isotopic composition from Proterozoic mafic rocks in north Qinling area and its implication. Chinese Science Bulletin,42(1):51-54.
    Xu, J. F., Zhang, B. R., Han, Y. W.2008. Geochemistry of the Mian-Lue ophiolites in the Qinhng Mountains, central China:Constraints on the evolution of the Qinling orogenic belt and collision of the North and South China Cratons. Journal of Asian Earth Sciences,32(5-6): 336-347.
    Xu, S. T., Okay, A. I., Ji, S. Y, Seng6r, A. M. C., Su, W., Liu, Y. C., Jiang, L. L.1992. Diamond from the Dabie Shan Metamorphic Rocks and Its Implication for Tectonic Setting. Science, 256(5053):80-82.
    Xu, X., Griffin, W. L., Ma, X., O'Reilly, S. Y, He, Z., Zhang, C.2009. The Taihua group on the southern margin of the North China craton:further insights from U-Pb ages and Hf isotope compositions of zircons. Mineralogy and Petrology,97(1-2):43-59.
    Xu, X., O'Reilly, S. Y, Griffin, W. L., Wang, X., Pearson, N. J., He, Z.2007. The crust of Cathaysia:Age, assembly and reworking of two terranes. Precambrian Research,158(1-2): 51-78.
    Xu, Z. Q.1987. Etude tectonigue et microtectonigue de la chaine paleozoique et triasique des Qinling (Chine). Academie de Montpellier University des Sciences et Techniques du Languedoc (unpublished PhD thesis), pp 96-98.
    Xue, F., Kroner, A., Reischmann, T., Lerch, F.1996a. Palaeozoic pre- and post-collision calc-alkaline magmatism in the Qinling orogenic belt, central China, as documented by zircon ages on granitoid rocks. Journal of the Geological Society,153:409-417.
    Xue, F., Lerch, M. F., Kroner, A., Reischmann, T.1996b. Tectonic evolution of the east Qinling Mountains, China, in the Palaeozoic:A review and new tectonic model. Tectonophysics, 253(3-4):271-284.
    Yan, Q., Wang, Z., Hanson, A. D., Druschke, P. A., Yan, Z., Liu, D., Jian, P., Song, B., Wang, T., Jiang, C.2003. SHRIMP age and Geochemistry of the Bikou volcanic terrane:implications for Neoproterozoic tectonics on the northern margin of the Yangtze craton. Acta Geologica Sinica-English Edition,77(4):479-490.
    Yan, Z., Wang, Z. Q., Wang, T., Yan, Q. R., Xiao, W. J., Li, J. L.2006a. Provenance and tectonic setting of clastic deposits in the Devonian Xicheng Basin, Qinling Orogen, central China. Journal of Sedimentary Research,76(3-4):557-574.
    Yan, Z., Wang, Z. Q., Yan, Q. R., Wang, T., Xiao, W. J., Li, J. L., Han, F. L., Chen, J. L., Yang, Y. C.2006b. Devonian sedimentary environments and provenance of the Qinling orogen: Constraints on late Paleozoic southward accretionary tectonics of the North China craton. International Geology Review,48(7):585-618.
    Yang, J. S., Xu, Z. Q., Zhang, J. X., Song, S. G, Wu, C. L., Shi, R. D., Li, H. B., Brunel, M.2002. Early Palaeozoic North Qaidam UHP metamorphic belt on the north-eastern Tibetan plateau and a paired subduction model. Terra Nova,14(5):397-404.
    Yang, J., Gao, S., Chen, C., Tang, Y, Yuan, H., Gong, H., Xie, S., Wang, J.2009. Episodic crustal growth of North China as revealed by U-Pb age and Hf isotopes of detrital zircons from modern rivers. Geochimica Et Cosmochimica Acta,73(9):2660-2673.
    Yang, J., Smith, D. C.1989. Evidence for a former sanidine-coesite eclogite at Lanshantou, eastern China, and the recognition of the Chinese "Su-Lu Coesite-Eclogite Province". Third International Eclogite Conference, Blackwell:Terra Nova Abstracts,1:26.
    Yang, J., Xu, Z., Dobrzhinetskaya, L. F., Green, H. W., Pei, X., Shi, R., Wu, C., Wooden, J. L., Zhang, J., Wan, Y., Li, H.2003. Discovery of metamorphic diamonds in central China:an indication of a> 4000-km-long zone of deep subduction resulting from multiple continental collisions. Terra Nova,15(6):370-379.
    Yang, J., Xu, Z., Song, S., Zhang, J., Wu, C., Shi, R., Li, H., Brunel, M.2001. Discovery of coesite in the North Qaidam Early Palaeozoic ultrahigh pressure (UHP) metamorphic belt, NW China. Comptes Rendus de l'Academie des Sciences-Series IIA-Earth and Planetary Science,333(11):719-724.
    Yang, J.-H., Wu, F.-Y., Chung, S.-L., Wilde, S. A., Chu, M.-F.2004. Multiple sources for the origin of granites:Geochemical and Nd/Sr isotopic evidence from the Gudaoling granite and its mafic enclaves, northeast China. Geochimica Et Cosmochimica Acta,68(21):4469-4483.
    Ye, K., Yao, Y, Katayama, I., Cong, B., Wang, Q., Maruyama, S.2000. Large areal extent of ultrahigh-pressure metamorphism in the Sulu ultrahigh-pressure terrane of East China:new implications from coesite and omphacite inclusions in zircon of granitic gneiss. Lithos, 52(1-4):157-164.
    Yong, S., Ziaping, Y, Kroner, A.1994. Geochemistry and single zircon geochronology of Archaean TTG gneisses in the Taihua high-grade terrain, Lushan area, central China. Journal of Southeast Asian Earth Sciences,10(3-4):227-233.
    Yu, J.-H., O'Reilly, S. Y, Wang, L., Griffin, W. L., Zhang, M., Wang, R., Jiang, S., Shu, L.2008. Where was South China in the Rodinia supercontinent? Precambrian Research,164(1-2): 1-15.
    Yu, J.-H., O'Reilly, S. Y, Wang, L., Griffin, W. L., Zhou, M.-F., Zhang, M., Shu, L.2010. Components and episodic growth of Precambrian crust in the Cathaysia Block, South China: Evidence from U-Pb ages and Hf isotopes of zircons in Neoproterozoic sediments. Precambrian Research,181(1-4):97-114.
    Yu, Z. P., Meng, Q. R.1995. Late Paleozoic Sedimentary and Tectonic Evolution of the Shangdan Suture Zone, Eastern Qinling, China. Journal of Southeast Asian Earth Sciences,11(3): 237-242.
    Yuan, H.-L., Gao, S., Dai, M.-N., Zong, C.-L., Gunther, D., Fontaine, G. H., Liu, X.-M., Diwu, C. 2008. Simultaneous determinations of U-Pb age, Hf isotopes and trace element compositions of zircon by excimer laser-ablation quadrupole and multiple-collector ICP-MS. Chemical Geology,247(1-2):100-118.
    Zhai, X. M., Day, H. W., Hacker, B. R., You, Z. D.1998. Paleozoic metamorphism in the Qinling orogen, Tongbai Mountains, central China. Geology,26(4):371-374.
    Zhang, B. R., Zhang, H. F., Zhao, Z. D., Ling, W. L.1996a. Geochemical subdivision and evolution of the lithosphere in east Qinling and adjacent regions-Implications for tectonics. Science in China (Series D),39(3):245-255.
    Zhang, C. L., Li, M., Wang, T., Yuan, H. L., Yan, Y. X., Liu, X. M., Wang, J. Q., Liu, Y.2004. U-Pb zircon geochronology and geochemistry of granitoids in the Douling Group in the Eastern Qinling. Acta Geologica Sinica-English Edition,78(1):83-95.
    Zhang, C., Liu, L., Wang, T., Wang, X., Li, L., Gong, Q., Li, X.2013. Granitic magmatism related to early Paleozoic continental collision in North Qinling. Chinese Science Bulletin,58(35): 4405-4410.
    Zhang, G W., Guo, A. L., Liu, F. T., Xiao, Q. H., Meng, Q. R.1996b. Three-dimensional architecture and dynamic analysis of the Qinling orogenic belt:Science in China (Series D), 26(Suppl.):1-6.
    Zhang, G W., Meng, Q. G, Lai, S. C.1995. Tectonics and Structure of Qinling Orogenic Belt. Science in China (Series B),38(11):1379-1394.
    Zhang, G. W., Meng, Q. G, Yu, Z. P., Sun, Y, Zhou, D. W., Guo, A. L.1996c. Orogenesis and dynamics of the Qinling orogen. Science in China (Series D),39(3):225-234.
    Zhang, G.-W., Bai, Y.-B., Sun, Y, Guo, A.-L., Zhou, D.-W., Li, T.-H.1985. Composition and evolution of the archaean crust in central Henan, China. Precambrian Research,27(1-3): 7-35.
    Zhang, H. F., Jin, L. L., Zhang, L., Harris, N., Zhou, L., Hu, S. H., Zhang, B. R.2007. Geochemical and Pb-Sr-Nd isotopic compositions of granitoids from western Qinling belt: Constraints on basement nature and tectonic affinity. Science in China Series D:Earth Sciences,50(2):184-196.
    Zhang, J. X., Meng, F. C.2006. Lawsonite-bearing eclogites in the north Qilian and north Altyn Tagh:Evidence for cold subduction of oceanic crust. Chinese Science Bulletin,51(10): 1238-1244.
    Zhang, J. X., Meng, F. C., Yang, J. S.2005. A New HP/LT Metamorphic Terrane in the Northern Altyn Tagh, Western China International Geology Review,47(4):371-386.
    Zhang, J., Yang, J., Xu, Z., Meng, F., Li, H., Shi, R.2002. Evidence for UHP metamorphism of eclogites from the Altun Mountains. Chinese Science Bulletin,47(9):751-755.
    Zhang, J., Zhang, Z., Xu, Z., Yang, J., Cui, J.2001a. Petrology and geochronology of eclogites from the western segment of the Altyn Tagh, northwestern China. Lithos,56(2-3):187-206.
    Zhang, K. J.1997. North and South China collision along the eastern and southern North China margins. Tectonophysics,270(1-2):145-156.
    Zhang, S.-B., Zheng, Y.-F., Wu, Y.-B., Zhao, Z.-F., Gao, S., Wu, F.-Y.2006a. Zircon isotope evidence for≥3.5 Ga continental crust in the Yangtze craton of China. Precambrian Research,146(1-2):16-34.
    Zhang, S.-B., Zheng, Y.-F., Wu, Y.-B., Zhao, Z.-F., Gao, S., Wu, F.-Y.2006b. Zircon U-Pb age and Hf-O isotope evidence for Paleoproterozoic metamorphic event in South China. Precambrian Research,151(3-4):265-288.
    Zhang, S.-B., Zheng, Y.-F., Wu, Y.-B., Zhao, Z.-F., Gao, S., Wu, F.-Y.2006c. Zircon U-Pb age and Hf isotope evidence for 3.8 Ga crustal remnant and episodic reworking of Archean crust in South China. Earth and Planetary Science Letters,252(1-2):56-71.
    Zhang, S.-B., Zheng, Y.-F., Zhao, Z.-F., Wu, Y.-B., Yuan, H., Wu, F.-Y.2008. Neoproterozoic anatexis of Archean lithosphere:Geochemical evidence from felsic to mafic intrusions at Xiaofeng in the Yangtze Gorge, South China. Precambrian Research,163(3-4):210-238.
    Zhang, Z. Q., Zhang, G. W., Fu, G. M., Tang, S. H., Song, B.1996d. Geochronology of metamorphic strata in the Qinling mountains and its tectonic implications. Science in China (Series D),39(3):283-292.
    Zhang, Z. Q., Zhang, G. W., Tang, S. H., Wang, J. H.2001b. Geochronology and geochemistry of the Heihe mafic pillow lavas in the Qinling Mountains, China. Science in China Series D: Earth Sciences,44(6):517-524.
    Zhao, J.-H., Zhou, M.-F.2008. Neoproterozoic adakitic plutons in the northern margin of the Yangtze Block, China:Partial melting of a thickened lower crust and implications for secular crustal evolution. Lithos,104(1-4):231-248.
    Zhao, J.-H., Zhou, M.-F.2009. Secular evolution of the Neoproterozoic lithospheric mantle underneath the northern margin of the Yangtze Block, South China. Lithos,107(3-4): 152-168.
    Zhao, J.-H., Zhou, M.-F., Zheng, J.-P., Fang, S.-M.2010a. Neoproterozoic crustal growth and reworking of the Northwestern Yangtze Block:Constraints from the Xixiang dioritic intrusion, South China. Lithos,120(3-4):439-452.
    Zhao, T.-P., Zhou, M.-F., Zhai, M., and Xia, B.2002. Paleoproterozoic Rift-Related Volcanism of the Xiong'er Group, North China Craton:Implications for the Breakup of Columbia. International Geology Review,44(4):336-351.
    Zhao, X.-F., Zhou, M.-F., Li, J.-W., Sun, M., Gao, J.-F., Sun, W.-H., Yang, J.-H.2010b. Late Paleoproterozoic to early Mesoproterozoic Dongchuan Group in Yunnan, SW China: Implications for tectonic evolution of the Yangtze Block. Precambrian Research,182(1-2): 57-69.
    Zheng, J., Griffin, W. L., O'Reilly, S. Y, Zhang, M., Pearson, N., Pan, Y.2006a. Widespread Archean basement beneath the Yangtze craton. Geology,34(6):417.
    Zheng, Y, Zhang, S.2007. Formation and evolution of Precambrian continental crust in South China. Chinese Science Bulletin,52(1):1-12.
    Zheng, Y.-F., Zhao, Z.-F., Wu, Y.-B., Zhang, S.-B., Liu, X., Wu, F.-Y. 2006b. Zircon U-Pb age, Hf and O isotope constraints on protolith origin of ultrahigh-pressure eclogite and gneiss in the Dabie orogen. Chemical Geology,231(1-2):135-158.
    Zhou, D. W., Zhang, C. L., Wang, J. L., Liu, L., Dong, Y. P., Liu, Y Y, Han, S.1998. The basic dyke swarms in the Wudang block and its geological significance. Chinese Science Bulletin, 43(13):1111-1115.
    Zhou, X., Sun, M., Zhang, G., Chen, S.2002. Continental crust and lithospheric mantle interaction beneath North China:isotopic evidence.from granulite xenoliths in Hannuoba, Sino-Korean craton. Lithos,62(3):111-124.
    Zhu, X. Y, Chen, F. K., Li, S. Q., Yang, Y. Z., Nie, H., Siebel, W., Zhai, M. G. 2011. Crustal evolution of the North Qinling terrain of the Qinling Orogen, China:Evidence from detrital zircon U-Pb ages and Hf isotopic composition. Gondwana Research,20(1):194-204.
    Zhu, X., Zhai, M., Chen, F., Lyu, B., Wang, W., Peng, P., Hu, B.2013. An~2.7-Ga Crustal Growth in the North China Craton:Evidence from Zircon U-Pb Ages and Hf Isotopes of the Sushui Complex in the Zhongtiao Terrane. The Journal of Geology,121(3):239-254.
    安三元,胡能高.1992.北秦岭裂陷的形成与变质作用.西安:西北大学出版社,pp 1-63.
    安三元,张维吉,杨家喜,林学军.1990.陕西太白地区秦岭群的岩石组合与编制作用.见:刘国惠和张寿广主编,秦岭-大巴山地质论文集(一)变质地质,北京:北京科学技术出版社,pp25-39.
    安三元,周廷梅,胡能高.1985.秦岭群的构造变形和变质史及其时代问题雏议.中国区域地质,13:87-93.
    安三元.1993.北秦岭地质新知及一些有关问题.西安地质学院学报,15(4):52-56.
    蔡志勇,罗洪,熊小林,吴德宽,吴贤亮,孙三才,杨军.2006.武当群上部变沉积岩组时代归属问题:单锆石U-Pb年龄的制约.地层学杂志,30(1):60-63.
    蔡志勇,熊小林,罗洪,吴德宽,孙三才,饶帮良,王寿琼.2007.武当地块耀岭河群火山岩的时代归属:单锆石U-Pb年龄的制约.地质学报,81(5):620-625.
    陈丹玲,刘良,孙勇,张安达,柳小明,罗金海.2004.北秦岭松树沟高压基性麻粒岩锆石的LA-ICP-MSU-Pb定年及其地质意义.科学通报,49(18):1901-1908.
    陈丹玲,刘良,王焰,罗金海.2001.秦岭杂岩残存高压不纯大理岩的确定及其意义.西北大学学报(自然科学版),31(4):324-328.
    陈丹玲,刘良,周鼎武,罗金海,桑海清.2002.东秦岭松树沟超镁铁质岩中辉石巨晶的成因和40Ar-39Ar定年及其地质意义.岩石学报,18(3):355-362.
    陈丹玲,刘良.2011.北秦岭榴辉岩及相关岩石年代学的进一步确定及其对板片俯冲属性的约束.地学前缘,18(2):158-169.
    陈江峰,江博明.1999. Nd、Sr、Pb同位素示踪和中国东南大陆地壳演化.见:郑永飞主编,化学地球动力学.北京:科学出版社,pp 262-287.
    陈隽璐,王宗起,徐学义,曾佐勋,王洪亮,何世平,李平.2007.北秦岭两河口岩体的地球化学特征及其成因.岩石学报,23(5):1043-1054.
    陈隽璐,徐学义,王宗起,闫全人,王洪亮,曾佐勋,李平.2008.西秦岭太白地区岩湾-鹦鸽咀蛇绿混杂岩的地质特征及形成时代.地质通报,27(4):500-509.
    陈隽璐,张占武,李海平,赵选社,宋红香.2004.秦岭杂岩中变质侵入体特征.西北地质,37(1):34-39.
    陈亮,孙勇,裴先治,冯涛,张国伟.2003.古特提斯蛇绿岩的综合对比及其动力学意义-以德尔尼蛇绿岩为例.中国科学(D辑:地球科学),33(12):1136-1142.
    陈亮,孙勇,裴先治,高明,冯涛,张宗清,陈文.2001.德尔尼蛇绿岩40Ar-39Ar年龄:青藏最北端古特提斯洋盆存在和延展的证据.科学通报,46(5):424-426.
    陈能松,巴金,张璐,苏文,刘景波,郭顺.2009.东秦岭商丹断裂带南侧武关岩群的锆石LA-ICP-MS U-Pb年龄.地质通报,28(5):556-560.
    陈能松,韩郁菁,游振东,孙敏.1991.豫西东秦岭造山带核部杂岩全岩Sm-Nd. Rb-Sr和单晶锆石207Pb-206Pb计时及其地壳演化.地球化学,20(3):219-228.
    陈能松,游振东,韩郁菁.1990.豫西东秦岭造山带核部杂岩变质作用研究若干进展.地质科技情报,9(3):20-24.
    陈能松.1990.豫西蛇尾秦岭群P-T轨迹定量计算及其地质意义.地球科学-中国地质大学学报,15(2):145-155.
    陈强,陈能松,王勤燕,孙敏,王新宇,李晓彦,舒桂明.2006.秦岭造山带秦岭岩群独居石电子探针化学年龄:晚泛非期变质证据?科学通报,51(21):2512-2516.
    陈衍景,富士谷,胡受奚,陈泽铭,周顺之.1991.华北克拉通南缘的地块差异性及其成矿意义:大地构造与成矿学,15(3):265-271.
    陈岳龙,杨忠芳,张宏飞,凌文黎.1996.北秦岭晚古生代—中生代花岗岩类的Nd, Sr, Pb同位素地球化学特征及Nd,Sr同位素演化.地球科学-中国地质大学学报,21(5):481-486.
    陈岳龙,张本仁,帕拉提·阿布都卡得尔.1995.北秦岭丹凤地区早古生代花岗岩的Pb、Sr、 Nd同位素地球化学特征.地质科学,30(3):248-258.
    陈岳龙.1999.东天山、北秦岭花岗岩类地球化学.北京:地质出版社,pp1-141.
    陈志宏,陆松年,李怀坤,宋彪,李惠民,相振群.2004a.北秦岭德河黑云二长花岗片麻岩体 的成岩时代-TIMS和SHRIMP锆石U-Pb同位素年代学.地质通报,23(2):136-141.
    陈志宏,陆松年,李怀坤,周红英,相振群,郭进京.2004b.秦岭造山带富水中基性侵入杂岩的成岩时代—锆石U-Pb及全岩Sm、Nd同位素年代学新证据.地质通报,23(4):322-328.
    崔建堂,韩芳林,张拴厚,王根宝,王北颖,王学平,彭海练,王金安,郭岐明,彭俟英,崔海曼.2010.南秦岭西乡群锆石SHRIMP U-Pb年龄及其构造地质意义.陕西地质,28(2):53-58.
    崔智林,孙勇,王学仁.1996.秦岭丹凤蛇绿岩带放射虫的发现及其地质意义.科学通报,40(18):1686-1688.
    邓晋福,肖庆辉,苏尚国,刘翠,赵国春,吴宗絮,刘勇.2007.火成岩组合与构造环境:讨论.高校地质学报,13(3):392-402.
    邓清禄,杨巍然.1996.秦岭造山带早古生代“开”“合”构造格局及加里东运动.地质科技情报,15(2):45-50.
    第五春荣,孙勇,林慈銮,王洪亮.2010a.河南鲁山地区太华杂岩LA-(MC)-ICPMS锆石U-Pb年代学及Hf同位素组成.科学通报,55(21):2112-2123.
    第五春荣,孙勇,刘良,张成立,王洪亮.2010b.北秦岭宽坪岩群的解体及新元古代N-MORB.岩石学报,26(7):2025-2038.
    第五春荣,孙勇,王倩.2012.华北克拉通地壳生长和演化:来自现代河流碎屑锆石Hf同位素组成的启示.岩石学报,28(11):3520-3530.
    第五春荣,孙勇,袁洪林,王洪亮,钟兴平,柳小明.2008.河南登封地区嵩山石英岩碎屑锆石U-Pb年代学、Hf同位素组成及其地质意义.科学通报,53(16):1923-1934.
    第五春荣.2010.华北克拉通南缘早前寒武纪地壳的形成和演化-太华、登封杂岩锆石U-Pb年代学及Hf同位素组成.博士论文:西北大学,pp 1-95.
    董申保,田伟.2007.花岗岩研究的反思.高校地质学报,13(3):353-361.
    董云鹏,杨钊,张国伟,赵霞,徐静刚,姚安平.2008.西秦岭关子镇蛇绿岩地球化学及其大地构造意义.地质学报,82(9):1186-1194.
    董云鹏,张国伟,赖绍聪,周鼎武,朱炳泉.1999.随州花山蛇绿构造混杂岩的厘定及其大地构造意义.中国科学(D辑:地球科学),29(3):222-231.
    董云鹏,张国伟,杨钊,赵霞,马海勇,姚安平.2007.西秦岭武山E-MORB型蛇绿岩及相关火山岩地球化学.中国科学(D辑:地球科学),37(增刊Ⅰ):199-208.
    董云鹏,张国伟,朱炳泉.2003.北秦岭构造属性与元古代构造演化.地球学报,24(1):3-10.
    董云鹏,周鼎武,刘良,张旗,张宗清.1997a.东秦岭松树沟蛇绿岩Sm-Nd同位素年龄的地质意义.中国区域地质,16(2):217-221.
    董云鹏,周鼎武,张国伟.1997b.东秦岭富水基性杂岩体地球化学特征及其形成环境.地球化学,26(3):79-88.
    高山,张本仁.1990.扬子地台北部太古宙TTG片麻岩的发现及其意义.地球科学-中国地质大学学报,15(6):675-679.
    郭安林,张国伟,孙延贵,郑健康,刘晔,王建其.2006.阿尼玛卿蛇绿岩带OIB和MORB的地球化学及空间分布特征:玛积雪山古洋脊热点构造证据.中国科学(D辑):地球科学,36(7):618-629.
    郭安林.1988.河南中部太古代登封花岗-绿岩地体中TTG质片麻岩与绿岩带关系及其地壳演化意义.地质论评,34(2):123-131.
    郭彩莲,陈丹玲,樊伟,王爱国.2010.豫西二郎坪满子营花岗岩体地球化学及年代学研究.岩石矿物学杂志,29(1):15-22.
    郭彩莲,陈丹玲.2011.豫西二郎坪地区O型埃达克岩的厘定及其地质意义.地质学报,85(12):1994-2002.
    何世平,王洪亮,陈隽璐,徐学义,张宏飞,任光明,余吉远.2007.北秦岭西段宽坪岩群斜长角闪岩锆石LA-ICP-MS测年及其地质意义.地质学报,81(1):79-87.
    和政军,牛宝贵,任纪舜.2005.陕南山阳地区刘岭群砂岩岩石地球化学特征及其构造背景分析.地质科学,40(4):594-607.
    侯振辉,王晨香.2007.电感耦合等离子体质谱法测定地质样品中35种微量元素.中国科学技术大学学报,37(8):940-944.
    胡国辉,赵太平,周艳艳,杨阳.2012b.华北克拉通南缘五佛山群沉积时代和物源区分析:碎屑锆石U-Pb年龄和Hf同位素证据.地球化学,41(4):326-342.
    胡国辉,周艳艳,赵太平.2012a.河南嵩山地区元古宙五佛山群沉积岩的地球化学特征及其对物源区和构造环境的制约.岩石学报,28(11):3692-3704.
    胡能高,王涛,杨家喜,赵东林.1994.东秦岭秦岭群中榴辉岩的发现及其地质意义.西安地质学院学报,16(2):105-106.
    胡能高,杨家喜,赵东林.1996.北秦岭榴辉岩Sm-Nd同位素年龄.矿物学报,16(4):349-352.
    胡能高,赵东林,徐柏青,王涛.1994b.北秦岭含柯石英榴辉岩的发现及其意义.科学通报,39(21):2013.
    胡能高,赵东林,徐柏青,王涛.1995.北秦岭官坡地区高压-超高压榴辉岩岩相学及变质作用研究.矿物岩石,15(4):1-9.
    黄汲清.1945.中国主要大地构造特征.中央地质调查所文集(甲种),20:1-165.
    黄萱,吴利仁.1990.陕西地区岩浆岩Nd、Sr同位素特征及其与大地构造发展的联系.岩石学报,2:1-11.
    姜春发,王宗起,李锦轶.2000.中央造山带开合构造.北京:地质出版社,pp 1-154.
    姜春发,张庆贵,张玉岫,朱志直.1963.东秦岭地槽型印支运动的存在.地质论评,21(3):1-10.
    姜春发.1993.中央造山带主要地质构造特征.地学研究,27:68-108.
    蒋宗胜,王国栋,肖玲玲,第五春荣,卢俊生,吴春明.2011.河南洛宁太华变质杂岩区早元古代变质作用P-T-t轨迹及其大地构造意义.岩石学报,27(12):3701-3717.
    赖绍聪,李三忠,张国伟.2003a.陕西西乡群火山-沉积岩系形成构造环境:火山岩地球化学约束.岩石学报,19(1):141-152.
    赖绍聪,张国伟,董云鹏,裴先治,陈亮.2003b.秦岭-大别勉略构造带蛇绿岩与相关火山岩性质及其时空分布.中国科学(D辑:地球科学),33(12):1174-1183.
    赖绍聪,张国伟,裴先治,杨海峰.2003c.南秦岭康县-琵琶寺-南坪构造混杂带蛇绿岩与洋岛火山岩地球化学及其大地构造意义.中国科学(D辑:地球科学),33(1):10-19.
    赖绍聪,张国伟,杨瑞瑛.2000.南秦岭巴山弧两河-饶峰-五里坝岛弧岩浆带的厘定及其大地构造意义.中国科学(D辑:地球科学),30(增刊):53-63.
    赖绍聪,张国伟,杨永成,陈家义.1997.南秦岭勉县-略阳结合带变质火山岩岩石地球化学特征.岩石学报,13(4):563-573.
    劳子强,王世炎.1999.河南省嵩山地区登封群研究的新进展.中国区域地质,18(1):9-16.
    雷敏.2010.秦岭造山带东部花岗岩成因及其与造山带构造演化的关系.博士论文:中国地质科学院,pp 1-161.
    李春麟.2011.小秦岭太华群花岗片麻岩与小河花岗岩形成时代及构造意义.硕士论文:中国地质大学,pp 1-50.
    李春昱,刘仰文,朱宝清,冯益民,吴汉泉.1978.秦岭及祁连山构造发展史.西北地质,(4):1-12.
    李福林,李益龙,周国华,徐士元,李祖刚,周汉文.2010.湖北随州大狼山群片岩中碎屑锆石的U-Pb年龄及其意义.岩石矿物学杂志,29(5):488-496.
    李红中,周永章,张连昌,何俊国,杨志军,梁锦,周留煜,瓦西拉里.2012.华北克拉通南部元古代熊耳群硅质岩地球化学及形成机制研究.岩石学报,28(11):3679-3691.
    李洪英,刘军锋,杨磊.2009.北秦岭松树沟超镁铁质岩体接触变质带中锆石特征及其地质意义.岩石矿物学杂志,28(3):225-234.
    李怀坤,陆松年,陈志宏,相振群,周红英,郝国杰.2003.南秦岭耀岭河群裂谷型火山岩锆石U-Pb年代学.地质通报,22(10):775-781.
    李惠民,陈志宏,相振群,李怀坤,陆松年,周红英,宋彪.2006.秦岭造山带商南-西峡地区富水杂岩的变辉长岩中斜锆石与锆石U-Pb同位素年龄的差异.地质通报,25(6):653-659.
    李平,陈隽璐,徐学义,王洪亮,李婷,高婷.2011.北秦岭武关岩体LA-ICPMS锆石U-Pb定年及岩石成因研究.岩石矿物学杂志,30(4):610-624.
    李曙光,Hart, S. R.,郭安林,张国伟.1987.河南中部登封群全岩Sm-Nd同位素年龄及其构 造意义.科学通报,22:1728-1731.
    李曙光,陈移之,张国伟,张宗清.1991.一个距今10亿年侵位的阿尔卑斯型橄榄岩体:北秦岭晚元古代板块构造体制的证据.地质论评,37(3):235-242.
    李曙光,侯振辉,杨永成,孙卫东,张国伟,李秋立.2003.南秦岭勉略构造带三岔子古岩浆弧的地球化学特征及形成时代.中国科学(D辑:地球科学),33(12):1163-1173.
    李王哗.2008.西秦岭—东昆仑造山带蛇绿岩及岛弧型岩浆岩的年代学和地球化学研究.博士论文:中国科学技术大学,pp 1-154.
    李文厚,梁金哲,邵磊,林晋炎.1991.陕西山阳地区刘岭群的风暴沉积和海底扇沉积.西北大学学报,21(1):95-99.
    李伍平,王涛,王晓霞,曹惠锋.2000.北秦岭灰池子复式岩体单颗粒锆石年龄.中国区域地质,19(2):172-174.
    李伍平,王涛,王晓霞.2001.北秦岭灰池子花岗质复式岩体的源岩讨论—元素-同位素地球化学制约.地球科学-中国地质大学学报,26(3):269-278.
    李先梓,严阵,卢欣祥等.1993.秦岭—大别山花岗岩.北京:地质出版社.pp 1-218.
    李献华,赵振华,桂训唐,于津生.1991.华南前寒武纪地壳形成时代的Sm-Nd和锆石U-Pb同位素制约.地球化学,(3):255-264.
    李亚林,张国伟,宋传中.1998.东秦岭二郎坪弧后盆地双向式俯冲特征.高校地质学报,4(3):286-293.
    李晔,周汉文,钟增球,向华,曾雯,祁冬梅,张利.2012.北秦岭早古生代两期变质作用:来自松树沟基性岩岩石学及锆石U-Pb年代学的记录.地球科学-中国地质大学学报,37(增刊):111-124.
    林慈銮.2006.河南鲁山地区太古代片麻岩系的地球化学、锆石年代学及其构造环境.硕士论文:西北大学,pp1-82.
    凌文黎,段瑞春,柳小明,程建萍,毛新武,彭练红,刘早学,杨红梅,任邦方.2010.南秦岭武当山群碎屑锆石U-Pb年代学及其地质意义.科学通报,55(12):1153-1161.
    凌文黎,高山,欧阳建平,张本仁,李惠民.2002.西乡群的时代与构造背景:同位素年代学及地球化学制约.中国科学(D辑:地球科学),32(2):101-112.
    凌文黎,任邦方,段瑞春,柳小明,毛新武,彭练红,刘早学,程建萍,杨红梅.2007.南秦岭武当山群、耀岭河群及基性侵入岩群锆石U-Pb同位素年代学及其地质意义.科学通报,52(12):1445-1456.
    凌文黎,周炼,张宏飞,欧阳建平.1996.扬子克拉通北缘元古宙基底同位素地质年代学和地壳增生历史:Ⅱ.火地垭群.地球科学-中国地质大学学报,21(5):495-500.
    凌文黎.1996.扬子克拉通北缘元古宙基底同位素地质年代学和地壳增生历史:Ⅰ.后河群和西乡群.地球科学-中国地质大学学报,21(5):491-494.
    刘丙祥,聂虎,齐玥,杨力,祝禧艳,陈福坤.2013.豫西南地区北秦岭地体新元古代花岗岩类岩石成因及其地质意义.岩石学报,29(07):2437-2455.
    刘春花,吴才来,郜源红,雷敏,秦海鹏,李名则.2013.南秦岭麻池河乡和沙河湾花岗岩体锆石LA-ICP-MS U-Pb年代学及Lu-Hf同位素组成.地学前缘,20:1-21.
    刘国惠,张寿广,游振东,索书田,张国伟.1993.秦岭造山带主要变质岩群及变质演化.北京:地质出版社,pp 1-190.
    刘会彬,裴先治,丁仨平,李佐臣,孙仁奇.2006.西秦岭天水市元龙地区新元古代花岗质片麻岩锆石LA-ICP-MS U-Pb定年及其地质意义.地质通报,25(11):1315-1320.
    刘军锋,孙勇,冯涛,胡艳华,孙卫东.2008.北秦岭四方台基性-超基性杂岩的地球化学特征及其成因.地球化学,37(2):174-186.
    刘军锋,孙勇,李洪英,杨磊.2012.北秦岭四方台基性-超基性杂岩锆石LA-ICP-MS年代学研究.岩石矿物学杂志,31(4):524-530.
    刘军锋,孙勇,孙卫东.2009.秦岭拉鸡庙镁铁质岩体锆石LA-ICP-MS年代学研究.岩石学报,25(2):320-330.
    刘军锋,孙勇.2005.东秦岭松树沟超基性岩体“热”侵位时代新知.地质论评,51(2):189-192.
    刘军锋.2008.秦岭商—丹构造带镁铁质、超镁铁质岩体研究及其地质意义.博士论文:西北大学,pp 1-127.
    刘良,曹玉亭,陈丹玲,张成立,杨文强,康磊,廖小莹.2013a.南阿尔金与北秦岭高压-超高压变质作用研究新进展.科学通报,58(22):2113-2123.
    刘良,陈丹玲,王超,张成立.2009.阿尔金、柴北缘与北秦岭高压-超高压岩石年代学研究进展及其构造地质意义.西北大学学报(自然科学版),39(3):472-479.
    刘良,陈丹玲,张安达,张成立,袁洪林,柳小明.2003.北秦岭高压-超高压变质岩的峰期变质时代及其地质意义.二十一世纪初构造地质学发展战略学术研讨会论文摘要,A96.
    刘良,廖小莹,张成立,陈丹玲,宫相宽,康磊.2013b.北秦岭高压-超高压岩石的多期变质时代及其地质意义.岩石学报,29(5):1634-1656.
    刘良,周鼎武,董云鹏,,张宏发,刘养杰,张泽军.1995.东秦岭松树沟高压变质基性岩石及其退变质作用的PTt演化轨迹.岩石学报,11(2):127-136.
    刘良,周鼎武,王焰,陈丹玲,刘雁.1996.东秦岭秦岭杂岩中的长英质高压麻粒岩及其地质意义初探.中国科学(D辑:地球科学),26(增刊):56-63.
    刘良,周鼎武.1994.东秦岭商南松树沟高压基性麻粒岩的发现及初步研究.科学通报,37(17):1599-1601.
    刘树文,杨朋涛,李秋根,王宗起,张万益,王伟.2011.秦岭中段印支期花岗质岩浆作用与造山过程.吉林大学学报(地球科学版),41(6):1928-1943.
    卢书炜.1994.南召县板山坪花岗质岩带地质特征与成因探讨.河南地质,12(3):190-197.
    卢欣祥,董有,尉向东,肖庆辉,李晓波,张宗清.1999.东秦岭吐雾山A型花岗岩的时代及其构造意义.科学通报,44(9):975-978.
    卢欣祥,肖庆辉,董有,李晓波,常秋玲.2000.秦岭花岗岩大地构造图.西安:西安地图出版社.
    卢欣祥.1987.东秦岭与蛇绿岩有关的幔源型(M-型)花岗岩的地质地球化学特征,刃:张国伟等主编,秦岭造山带的形成与演化.西安:西北大学出版社,pp 149-162.
    卢欣祥.1998.秦岭花岗岩揭示的秦岭构造演化过程—秦岭花岗岩研究进展.地球科学进展,13(2):213-214.
    卢欣祥.2004.秦岭花岗岩与秦岭造山带构造演化关系.2004年全国岩石学与地球动力学研讨会论文摘要集,A149-150.
    鲁祖惠,胥爱军,陈冬荣,王玉金,李友明,郭士伦,郝秀红,关保德,陶自强.1994.栾川群强烈热事件终止时间的确定.郑州大学学报(自然科学版),26(1):51-55.
    陆松年,陈志宏,李怀坤,郝国杰,相振群.2005.秦岭造山带中两条新元古代岩浆岩带.地质学报,79(2):165-173.
    陆松年,陈志宏,李怀坤,郝国杰,周红英,相振群.2004.秦岭造山带中一新元古代(早期)地质演化.地质通报,23(2):107-112.
    陆松年,陈志宏,相振群,李怀坤,李惠民,宋彪.2006.秦岭岩群副变质岩碎屑锆石年龄谱及其地质意义探讨.地学前缘,13(6):303-310.
    陆松年,李怀坤,陈志宏,郝国杰,周红英,郭进京,牛广华,相振群.2003.秦岭中-新元古代地质演化及对RODINIA超级大陆事件的响应.北京:地质出版社,pp 1-194.
    陆松年.2001.从罗迪尼亚到冈瓦纳超大陆-对新元古代超大陆研究几个问题的思考.地学前缘(中国地质大学,北京),8(4):441-448
    马杏垣,索书田,游振东.1981.嵩山构造变形重力构造、构造解析.北京:地质出版社,pp1-256.
    孟芳,毛景文,叶会寿,周珂,高亚龙,李永峰.2012.豫西老君山花岗岩体SHRIMP锆石U-Pb年龄及其地球化学特征.中国地质,39(6):1501-1524.
    孟芳.2010.豫西老君山花岗岩体特征及其成矿作用.硕士论文:中国地质大学(北京),ppl-76.
    孟庆任,梅志超,于在平,崔智林.1995.秦岭板块北缘一个消失了的泥盆纪古陆.科学通报,40(3):254-256.
    孟庆任,薛峰,张国伟.1994.秦岭商丹带内黑河地区砾岩沉积及其构造意义.沉积学报,12(3):37-46.
    孟庆任,于在平,梅志超.1997.北秦岭南缘弧前盆地沉积作用及盆地发展.地质科学,32(4):136-145.
    莫宣学,罗照华,邓晋福,喻学惠,刘成东,谌宏伟,袁万明,刘云华.2007.东昆仑造山带花岗岩及地壳生长.高校地质学报,13(3):403-414.
    倪志耀,王仁民,童英,杨淳,戴潼谟.2003.河南洛宁太华岩群斜长角闪岩的锆石207Pb/206Pb和角闪石40Ar/39Ar年龄.地质论评,49(4):361-366.
    倪智勇,李诺,张辉,薛良伟.2009.河南大湖金钼矿床成矿物质来源的锶钕铅同位素约束.岩石学报,25(11):2823-2832.
    欧阳建平,张本仁.1996.北秦岭微古陆形成与演化的地球化学证据.中国科学(D辑),26(增刊):42-48.
    裴先治,丁仨平,张国伟,刘会彬,李佐臣,李王晔,刘战庆,孟勇.2007.西秦岭北缘新元古代花岗质片麻岩的LA-ICP-MS锆石U-Pb年龄及其地质意义.地质学报,81(6):772-786.
    裴先治,胡能高,高进龙,李荣西,赵东林.1993.北秦岭富水杂岩体的变形构造及其侵位机制.西安地质学院学报,15(3):7-14.
    裴先治,李厚民,李国光,张维吉,王全庆,李志昌.1997a.东秦岭“武关岩群”斜长角闪岩Sm-Nd同位素年龄及其地质意义.中国区域地质,16(1):38-42.
    裴先治,李厚民,李国光,张维吉,王全庆.1997b.北秦岭富水基性杂岩体岩石谱系单位划分及演化.中国区域地质,16(3):231-238.
    裴先治,李厚民,李国光.2001.东秦岭丹凤岩群的形成时代和构造属性.岩石矿物学杂志,20(2):180-188.
    裴先治,王涛,王洋,李厚民,李国光.1999.北秦岭晋宁期主要地质事件及其构造背景探讨.高校地质学报,5(2):137-147.
    裴先治,王洋,.王涛.1998.北秦岭前寒武纪地壳组成及其构造演化.前寒武纪研究进展,21(4):26-35.
    裴先治.1997.东秦岭商丹构造带的组成与构造演化.西安:西安地图出版社,pp 1-133.
    钱加慧,杨秀清,刘良,曹玉亭,陈丹玲,杨文强.2013.北秦岭松树沟榴闪岩锆石U-Pb定年、矿物包裹体和Lu-Hf同位素特征及其地质意义.岩石学报,29(9):3087-3098.
    秦江峰,赖绍聪,张国伟,第五春荣,李永飞.2008.川贝九寨沟地区隆康熔结凝灰岩锆石LA-ICP-MS U-Pb年龄.地质通报,27(3):345-350.
    秦江峰,赖绍聪.2011.秦岭造山带晚三叠世花岗岩成因与深部动力学.北京:科学出版社,pp 1-267.
    秦克令,邹湘华,何世平,宋述光.1990.西秦岭鱼洞子群的建立和时代归属,见:刘国惠和张寿广主编,秦岭-大巴山地质论文集(一)变质地质,北京:北京科学技术出版社,pp167-175.
    任纪舜,牛宝贵,刘志刚.1999.软碰撞、叠覆造山和多旋回缝合作用.地学前缘(中国地质大学,北京),6(3):85-93.
    任纪舜,张正坤,牛宝贵,刘志刚.1991.论秦岭造山带-中朝与扬子陆块的拼合过程,见叶连俊等主编,秦岭造山带学术讨论会论文选集.西安:西北大学出版社,pp 99-110.
    尚瑞钧,严阵.1988.秦巴花岗岩.武汉:中国地质大学出版社,pp 1-229.
    沈洁,张宗清,刘敦一.1997.秦岭陡岭群变质杂岩Sm-Nd、Rb-Sr、40Ar/39Ar、207Pb/206Pb年龄.地球学报,18(3):248-254.
    时毓,于津海,徐夕生,邱检生,陈立辉.2009.秦岭造山带东段秦岭岩群的年代学和地球化学研究.岩石学报,25(10):2651-2670.
    时毓,于津海,徐夕生,唐红峰,邱检生,陈立辉.2011.陕西小秦岭地区太华群的锆石U-Pb年龄和Hf同位素组成.岩石学报,27(10):3095-3108.
    宋述光,苏犁,杨合群,王懿圣.1998.陕西商南松树沟橄榄岩体的成因及侵位机制.岩石学报,14(2):212-221.
    苏犁,宋述光,宋彪,周鼎武,郝建荣.2004.松树沟地区石榴辉石岩和富水杂岩SHRIMP锆石U-Pb年龄及其对秦岭造山带构造演化的制约.科学通报,49(12):1209-1211.
    苏犁,宋述光,周鼎武.2005.秦岭造山带松树沟纯橄岩体成因:地球化学和岩浆包裹体的制约.中国科学(D辑:地球科学),35(1):38-47.
    苏文,刘景波,陈能松,郭顺,巴金,张璐,刘新,施雨新.2013.东秦岭-大别山及其两侧的岩浆和变质事件年代学及其形成的大地构造背景.岩石学报,29(5):1573-1593.
    孙枢,张国伟,陈志明.1985.华北断块区南部前寒武纪地质演化.北京:冶金工业出版社,pp 1-216.
    孙卫东,李曙光,孙勇,张国伟,张宗清.1996.北秦岭西峡二郎坪群枕状熔岩中一个岩枕的年代学和地球化学研究.地质论评,42(2):144-153.
    孙卫东,李曙光,肖益林,孙勇,张国伟.1995.北秦岭黑河丹凤群岛弧火山岩建造的发现及其构造意义.大地构造与成矿学,19(3):227-236.
    孙勇,张国伟,杨司祥,卢欣祥,韩松.1996.北秦岭早古生代二郎坪蛇绿岩片的组成和地球化学.中国科学(D辑:地球科学),26(增刊):49-55.
    孙勇.1983.河南鲁山太华群的麻粒岩相变质岩.西北大学学报(自然科学版),1:92-98.
    孙勇.1991.东秦岭古洋盆与加里东运动.地质论评,37(6):555-559.
    索书田,钟增球,周汉文,游振东.2004.中国中央造山带内两个超高压变质带关系.地质学报,78(2):156-165.
    汤清龙,赵志强,吉恒召,杨涛,牛磊.2010.东秦岭二郎坪群地质特征及成矿规律.华南地质与矿产,4:45-54.
    汤耀庆,卢一伦.1986.东秦岭蛇绿岩的形成时代和构造环境.成都地质学院学报,13(2):52-65.
    陶洪祥,陈祥荣,冯鸿儒,吴兆星.1982.汉南“西乡群”的地层划分与对比.长安大学学报(地 球科学版),(1):31-44.
    田伟.2003.东秦岭加里东期花岗岩的区域岩石成因和大地构造环境.博士论文:北京大学,pp 1-68.
    万渝生,刘敦一,董春艳,殷小艳.2011.西峡北部秦岭群变质沉积岩锆石SHRIMP定年:物源区复杂演化历史和沉积、变质时代确定.岩石学报,27(4):1172-1178.
    万渝生,刘敦一,王世炎,赵逊,董春艳,周红英,殷小艳,杨长秀,高林志.2009.登封地区早前寒武纪地壳演化一地球化学和锆石SHRIMP U-Pb年代学制约.地质学报,83(7):982-999.
    王德滋,舒良树.2007.花岗岩构造岩浆组合.高校地质学报,13(3):362-370.
    王国栋,王浩,陈泓旭,卢俊生,肖玲玲,吴春明.2012.华北中部造山带南缘华山地区太华变质杂岩中锆石U-Pb定年.地质学报,86(9):1541-1551.
    王洪亮,徐学义,陈隽璐,闫臻,李婷,朱涛.2011.南秦岭略阳鱼洞子岩群磁铁石英岩形成时代的锆石U-Pb年代学约束,地质学报,85(8):1284-1290.
    王锦,第五春荣,孙勇,刘晔,王维.2012.豫西西峡地区青岗坪花岗闪长岩LA-ICP-MS锆石U-Pb测年、Hf同位素组成及其地质意义.地质通报,31(6):884-895.
    王清晨,孙枢,李继亮,周达,许靖华,张国伟.1989.秦岭的大地构造演化.地质科学,(2):129-142.
    王涛,胡能高,裴先治,杨家喜,李伍平.1997.秦岭杂岩的组成、构造格局及演化.地球学报,18,(4):345-351.
    王涛,李伍平,王晓霞.1998.秦岭杂岩牛角山花岗质片麻岩体锆石U-Pb同位素年龄及其地质意义.中国区域地质,17(3):262-265.
    王涛,王晓霞,郑亚东,洪大卫,王新社.2007.花岗岩构造研究及花岗岩构造动力学刍议.地质科学,42(1):91-113.
    王涛,张国伟,王晓霞,李伍平.1999.花岗岩体生长方式及构造运动学、动力学意义—以东秦岭造山带核部花岗岩体为例.地质科学,34(3):326-335.
    王涛,张宗清,王晓霞,王彦斌,张成立.2005.秦岭造山带核部新元古代碰撞变形及其时代一强变形同碰撞花岗岩与弱变形脉体锆石SHRIMP年龄限定.地质学报,79(2):220-232.
    王希斌,杨经绥,史仁灯,陈松永.2005.秦岭松树沟岩体一一个遭受角闪岩相变质作用的超镁铁堆晶岩的实例.地质学报,79(2):174-189.
    王晓霞,王涛,齐秋菊,李舢.2011.秦岭晚中生代花岗岩时空分布、成因演变及构造意义.岩石学报,27(6):1573-1593.
    王学仁,华洪,孙勇.1995.河南西峡湾潭地区二郎坪群微体化石研究.西北大学学报(自然科学版),25(4):353-358.
    王宗起,陈海泓,李继亮,郝杰,赵越,韩芳林,郝俊武.1998.南秦岭西乡群发现晚古生代 放射虫化石.地质论评,(3):263.
    王宗起,陈海泓,李继亮,郝杰,赵越,韩芳林,郝俊武.1999.南秦岭西乡群放射虫化石的发现及其地质意义.中国科学(D辑:地球科学),29(1):38-44.
    王宗起,高联达,王涛,姜春发.2007.北秦岭陶湾群新发现的微体化石及其对地层时代的限定.中国科学(D辑:地球科学),37(11):1467-1473.
    王宗起,王涛,闫臻,闫全人.2002.秦岭晚古生代弧前增生的背驮型盆地体系.地质通报,21(8-9):456-464.
    王宗起,闫臻,王涛,高联达,闫全人,陈隽璐,李秋根,姜春发,刘平,张英利,谢春林,向忠金.2009.秦岭造山带主要疑难地层时代研究的新进展.地球学报,30(5):561-570.
    魏春景,杨崇辉,张寿广,李荣社.1998.南秦岭佛坪地区麻粒岩的发现及其地质意义.科学通报,43(9):982-985.
    吴福元,李献华,郑永飞,高山.2007b. Lu-Hf同位素体系及其岩石学应用.岩石学报,23(2):185-220.
    吴福元,李献化,杨进辉,郑永飞,2007a.花岗岩成因研究的若干问题.岩石学报,23(6):1217-1238.
    吴元保.2009.大陆造山过程的多期演化:以西大别为例.科学通报,54(13):1815-1825.
    吴正文,柴育成,黄万夫,贾维民,王自强,张长厚.1991.秦岭中的的推覆构造格局,见:叶连俊等主编,秦岭造山带学术讨论会论文选集.西安:西北大学出版社,pp 111-120.
    夏林圻,夏祖春,马中平,徐学义,李向民.2009.南秦岭中段西乡群火山岩岩石成因.西北地质,42(2):1-37.
    夏林圻,夏祖春,徐学义,李向民,马中平.2007.碧口群火山岩岩石成因研究.地学前缘,14(3):84-101.
    夏林圻,夏祖春,徐学义.1996.南秦岭元古宙西乡群大陆溢流玄武岩的确定及其地质意义.地质论评,42(6):513-522.
    向华.2012.北秦岭一桐柏造山带早古生代多期次变质作用及构造演化.博士论文:中国地质大学,pp 1-196.
    肖庆辉,邓晋福,邱瑞照,刘勇,冯艳芳.2009.花岗岩类与大陆地壳生长初探-以中国典型造山带花岗岩类岩石的形成为例.中国地质,36(3):594-622.
    肖思云,张维吉,宋子季.1988.北秦岭变质地层.西安:西安交通大学出版社,pp 1-320.
    肖序常,陈国铭,朱志直.1978.祁连山古蛇绿岩带的地质构造意义.地质学报,52(4):281-296.
    徐贵忠,王艺芬.1990.论东秦岭前寒武纪的构造演化特征.地质科学,2:101-112.
    徐学义,陈隽璐,李向民,马中平,王洪亮,夏林圻,夏祖春,李平.2010.西乡群三郎铺组和大石沟组火山岩U-Pb定年及岩石成因研究.岩石学报,26(2):617-632.
    徐学义,夏林圻,陈隽璐,马中平,李向民,夏祖春,王洪亮.2009.扬子地块北缘西乡群孙家河组火山岩形成时代及元素地球化学研究.岩石学报,25(12):3309-3326.
    徐勇航,赵太平,陈伟.2009.东秦岭二郎坪群长英质火山岩成因及其对VMS型矿床成矿环境的制约.岩石学报,25(2):399-412.
    许继锋,韩吟文.1996.秦岭古MORB型岩石的高放射性成因铅同位素组成-特提斯型古洋幔存在的证据.中国科学(D辑:地球科学),26(增刊):34-41.
    许志琴,卢一伦,汤耀庆,张治洮.1988.东秦岭复合山链的形成-变形、演化及板块动力学.北京:中国环境科学出版社,pp 1-193.
    许志琴,牛宝贵,刘志刚.1991.秦岭-大别“碰撞-陆内”型复合山链的构造体制及陆内板块动力学机制,见叶连俊等主编,秦岭造山带学术讨论会论文选集.西安:西北大学出版社,pp 139-147.
    许志琴,杨经绥,李海兵,姚建新.2006.中央造山带早古生代地体构架与高压/超高压变质带的形成.地质学报,80(12):1793-1806.
    薛锋,张国伟.1993.秦岭造山带丹凤变质岛弧火山岩系的岩石组合与地球化学特征.地球化学,(1):80-92.
    薛良伟,张天义,徐莉,卢欣祥.2004.登封群的定年及其划分问题的探讨.地球学报,25(2):229-234.
    闫全人,陈隽璐,王宗起,闫臻,王涛,李秋根,张宗清,姜春发.2007b.北秦岭小王涧枕状熔岩中淡色侵入岩的地球化学特征、SHRIMP年龄及地质意义.中国科学(D辑:地球科学),37(10):1301-1313.
    闫全人,王宗起,陈隽璐,闫臻,王涛,李秋根,姜春发,张宗清.2007a.北秦岭斜峪关群和草滩沟群火山岩成因的地球化学和同位素约束、SHRIMP年代及其意义.地质学报,81(4):488-500.
    闫全人,王宗起,闫臻,王涛,陈隽璐,向忠金,张宗清,姜春发.2008.秦岭造山带宽坪群中的变铁镁质岩的成因、时代及其构造意义.地质通报,27(9):1475-1492.
    闫全人,王宗起,闫臻,向忠金,王涛,张宏远.2009.秦岭岩群中两类斜长角闪岩的性质和时代及其地质意义.岩石学报,25(9):2177-2194.
    闫臻,王宗起,王涛,闫全人,肖文交,李继亮,韩芳林,陈隽璐.2007.秦岭造山带泥盆系形成构造环境:来自碎屑岩组成和地球化学方面的约束.岩石学报,23(5):1023-1042.
    燕长海,徐勇航,彭翼,赵太平.2008.东秦岭二郎坪群中火山成因块状硫化物矿床地质地球化学特征及其成因讨论.矿床地质,27(1):14-27.
    杨斌虎,张成立,李雷.2011.东秦岭陡岭杂岩花岗岩的Sr-Nd-Pb同位素特征及其地质意义.地质通报,30(2-3):439-447.
    杨崇辉,魏春景,张寿广,李惠民,万渝生,李荣社.1999.南秦岭佛坪地区麻粒岩相岩石锆 石U-Pb年龄.地质论评,45(2):173-179.
    杨崇辉,张寿广,张宗清.1992.陕西户县沙坪古花岗岩体的特征和意义.中国地质科学院地质研究所所刊,25:127-136.
    杨经绥,刘福来,吴才来,万渝生,张建新,史仁灯,陈松永.2003.中央碰撞造山带中两期超高压变质作用来自含柯石英锆石的定年证据.地质学报,77(4):463-477.
    杨经绥,宋述光,许志琴,吴才来,史仁灯,张建新,李海兵,万渝生,刘焰,邱海峻,刘福来,Maruyama, S.2001.柴达木盆地北缘早古生代高压—超高压变质带中发现典型超高压矿物—柯石英.地质学报,75(2):175-179.
    杨经绥,许志琴,马昌前,吴才来,张建新,王宗起,王国灿,张宏飞,董云鹏,赖绍聪.2010.复合造山作用和中国中央造山带的科学问题.中国地质,37(1):1-11.
    杨经绥,许志琴,裴先治,史仁灯,吴才来,张建新,李海兵,孟繁聪,戎合.2002.秦岭发现金刚石:横贯中国中部巨型超高压变质带新证据及古生代和中生代两期深俯冲作用的识别.地质学报,76(4):484-495.
    杨经绥,许志琴,张建新,张泽明,刘福来,吴才来.2009.中国主要高压-超高压变质带的大地构造背景及俯冲/折返机制的探讨.岩石学报,25(7):1529-1560.
    杨力,陈福坤,杨一增,李双庆,祝禧艳.2010.丹凤地区秦岭岩群片麻岩锆石U-Pb年龄:北秦岭地体中-新元古代岩浆作用和早古生代变质作用的记录.岩石学报,26(5):1589-1603.
    杨森楠.1985.秦岭古生代陆间裂谷系的演化.地球科学-武汉地质学院学报,10(4):53-62.
    杨巍然,邓清录.1991.扬子克拉通与秦岭造山带的构造关系及金刚石矿的找寻.地质科技情报,10(增刊):135-140.
    杨巍然,杨森楠.1991.造山带结构与演化的现代理论和研究方法:东秦岭造山带剖析.武汉:中国地质大学出版社,pp 1-191.
    杨宗让.1999.中秦岭地区晚古生代增生的弧前构造带及演化初析.陕西地质,17(2):1-6.
    游振东,索书田,韩郁菁,钟增球,陈能松.1991.造山带核部杂岩变质过程与构造解析—以东秦岭为例.武汉:中国地质大学出版社,pp1-326.
    于红.2011.陕西商南松树沟橄榄岩矿物地球化学特征及成因机理示踪.硕士论文:中国地质大学(北京),pp1-67.
    于在平,孙勇,张国伟.1988.商丹地区秦岭缝合带弧前沉积楔形体初探,见:张国伟主编,秦岭造山带的形成及其演化.西安:西北大学出版社,pp75-85.
    于在平,孙勇,张国伟.1991.秦岭商丹缝合带沉积岩系基本地质特征,见:叶连俊等主编,秦岭造山带学术讨论会论文选集.西安:西北大学出版社,pp 78-88.
    张安达,刘良,王焰,陈丹玲,罗金海.2003.北秦岭榴辉岩的地球化学特征及形成环境.西北大学学报(自然科学版),33(2):191-195.
    张本仁,高山,张宏飞,韩吟文.2002.秦岭造山带地球化学.北京:科学出版社,pp 1-187.
    张本仁,韩吟文,许继锋,欧阳建平.1998.北秦岭新元古代前属于扬子板块的地球化学证据.高校地质学报,4(4):369-381.
    张本仁,骆庭川,高山,欧阳建平,陈德兴,马振东,韩吟文,谷晓明.1994.秦巴岩石圈构造及成矿规律地球化学研究.武汉:中国地质大学出版社,pp 1-446.
    张成立,刘良,张国伟,王涛,陈丹玲,袁洪林,柳小明,晏云翔.2004a.北秦岭新元古代后碰撞花岗岩的确定及其构造意义.地学前缘(中国地质大学,北京),11(3):33-42.
    张成立,王涛,王晓霞.2008.秦岭造山带早中生代花岗岩成因及其构造环境.高校地质学报,14(3):304-316.
    张成立,张国伟,刘爽,王守敬,周鼎武,刘良.2004b.东秦岭宽坪岩群变质火山碎屑岩及碎屑岩LA-ICPMS锆石U—-Pb年龄及其地质意义.2004年全国岩石学与地球动力学研讨会论文摘要集,A355-358.
    张成立,周鼎武,韩松.1994.陕西商州地区丹凤变质火山岩的地球化学特征.地质科学,29(4):384-392.
    张二朋,牛道韫,霍有光,张兰芳,李益桂.1993.秦巴及邻区地质-构造特征概论.北京:地质出版社,pp1-291.
    张国伟,董云鹏,赖绍聪,郭安林,孟庆任,刘少峰,程顺有,姚安平,张宗清,裴先治,李三忠.2003.秦岭-大别造山带南缘勉略构造带与勉略缝合带.中国科学(D辑:地球科学),33(12):1121-1135.
    张国伟,孙勇,于在平,薛峰.1988.北秦岭古活动大陆边缘,见:张国伟主编,秦岭造山带的形成及其演化.西安:西北大学出版社,pp 48-64.
    张国伟,于在平,董云鹏,姚平安.2000.秦岭区前寒武纪构造格局与演化问题探讨.岩石学报,16(1):11-21.
    张国伟,张本仁,袁学诚,肖庆辉.2001.秦岭造山带与大陆动力学.北京:科学出版社,pp1-855.
    张国伟,张宗清,董云鹏.1995.秦岭造山带主要构造岩石地层单元的构造性质及其大地构造意义.岩石学报,11(2):101-114.
    张国伟,周鼎武,周立法.1982.嵩箕地区前嵩山群古构造基本特征.西北大学学报(自然科学版),12(前寒武纪地质专集):12-22.
    张国伟,周鼎武.1990.秦岭杂岩和秦岭造山带.刃:刘国惠和张寿广主编,秦岭-大巴山地质论文集(一)变质地质,北京:北京科学技术出版社,pp11-24.
    张国伟.1988.秦岭造山带的形成及其演化.西安:西北大学出版社,pp1-192.
    张宏飞,骆庭川,张本仁.1994.北秦岭灰池子花岗岩基成岩物质来源探讨.矿物岩石,14(1):67-73.
    张宏飞,骆庭川,张本仁.1996.北秦岭漂池岩体的源区特征及其形成的构造环境.地质论评,42(3):209-214.
    张宏飞,张本仁,骆庭川.1993.北秦岭新元古代花岗岩类成因与构造环境的地球化学研究.地球科学-中国地质大学学报,18(2):194-202.
    张宏飞,赵志丹,骆庭川,张本仁.1995.从岩石Sm-Nd同位素模式年龄论北秦岭地壳增生和地壳深部性质.岩石学报,11(2):160-170.
    张宏飞.1992.扬子克拉通北缘和北秦岭古陆边缘花岗岩类形成与演化的地球化学研究.博士论文:中国地质大学,pp 1-88.
    张建新,于胜尧,孟繁聪,李金平.2009.造山带中成对出现的高压麻粒岩与榴辉岩及其地球动力学意义.岩石学报,25(9):2050-2066.
    张建新,于胜尧,孟繁聪.2011.北秦岭造山带的早古生代多期变质作用.岩石学报,27(4):1179-1190.
    张旗,张宗清,孙勇,韩松.1995.陕西商县-丹凤地区丹凤群变质玄武岩的微量元素和同位素地球化学.岩石学报,11(1):43-54.
    张秋生,朱永正.1984.东秦岭古生代蛇绿岩套.长春地质学院学报,(3):1-13.
    张秋生.1980.中国东秦岭变质地质.长春:吉林人民出版社,pp 1-223.
    张瑞英,张成立,孙勇.2013.华北克拉通-2.5Ga地壳再造事件:来自中条山TTG质片麻岩的证据.岩石学报,29(7):2265-2280.
    张少兵.2008.扬子陆核古老地壳及其深熔产物花岗岩的地球化学研究.博士论文:中国科学技术大学,pp 1-211.
    张寿广,张宗清,宋彪,唐索寒,赵子然,王进辉.2004.东秦岭陡岭杂岩中存在新太古代物质组成-SHRIMP锆石U-Pb和Sm-Nd年代学证据.地质学报,78(6):800-806.
    张维吉,王全庆,胡能高.1996.东秦岭地质走廊研究.西安:陕西科学技术出版社,pp 1-222.
    张欣,徐学义,宋公社,王洪亮,陈隽璐,李婷.2010.西秦岭略阳地区鱼洞子杂岩变形花岗岩锆石LA-ICP-MS U-Pb测年及地质意义.地质通报,29(4):510-517.
    张泽军,安三元.1992.松树沟超镁铁岩成因的地球化学证据.地球化学,(2):175-181.
    张泽军.1991.富水杂岩体地球化学特征及成因探讨.西安地质学院学报,13(2):14-22.
    张泽军.1995.北秦岭松树沟超镁铁质岩中两类不同成因的纯橄岩.岩石学报,11(增刊):178-189.
    张正伟,朱炳泉,常向阳.2000.东秦岭北部富碱侵入岩钕、锶、铅同位素特征及构造意义.地球化学,29(5):455-461.
    张宗清,黎世美.1998.河南省西部熊耳山地区太古宙太华群变质岩的Sm-Nd, Rb-Sr年龄及其地质意义,刃:程裕淇主编,华北地台早前寒武纪地质研究论文集.北京:地质出版社,pp 123-132.
    张宗清,刘敦一,付国民.1994.北秦岭变质地层同位素年代研究.北京:地质出版社,pp1-191.
    张宗清,宋彪,唐索寒,张寿广,杨永成,王进辉.2004.秦岭佛坪变质结晶岩系年龄和物质组成特征-SHRIMP锆英石U-Pb年代学和全岩Sm-Nd年代学数据.中国地质,31(2):161-168.
    张宗清,张国伟,刘敦一,王宗起,王进辉.2006.秦岭造山带蛇绿岩、花岗岩和碎屑沉积岩同位素年代学和地球化学.北京:地质出版社,pp 1-348.
    张宗清,张国伟,唐索寒,王进辉.2001.鱼洞子群变质岩年龄及秦岭造山带太古宙基底.地质学报,75(2):198-204.
    张宗清,张国伟,唐索寒,王进辉.2002a.武当群变质岩年龄.中国地质,29(2):117-125.
    张宗清,张国伟,唐索寒.2002b.南秦岭变质地层同位素年代学.北京:地质出版社,pp1-256.
    赵凤清,赵文平,左义成,李宗会,薛克勤.2006.陕南汉中地区新元古代岩浆岩U-Pb年代学.地质通报,25(3):383-388.
    赵姣,陈丹玲,谭清海,陈淼,朱小辉,郭彩莲,刘良.2012.秦岭东段二郎坪群火山岩锆石的LA-ICP-MS U-Pb定年及其地质意义.地学前缘,19(4):118-125.
    赵姣.2012.北秦岭东段二郎坪群火山岩的地球化学及年代学研究.硕士论文:西北大学,pp1-63.
    赵太平,徐勇航,翟明国.2007.华北陆块南部元古宙熊耳群火山岩的成因与构造环境:事实与争议.高校地质学报,13(2):191-206.
    赵太平,翟明国,夏斌,李惠民,张毅星,万渝生.2004.熊耳群火山岩锆石SHRIMP年代学研究:对华北克拉通盖层发育初始时间的制约.科学通报,49(22):2342-2394.
    赵子然,万渝生,张寿广,魏春景.1995.早元古陡岭群变质杂岩的岩石地球化学特征.岩石学报,11(2):148-159.
    郑永飞.2008.超高压变质与大陆碰撞研究进展:以大别-苏鲁造山带为例.科学通报,53(18):2129-2152.
    周鼎武,张成立,韩松,张泽军,董云鹏.1995a.东秦岭早古生代两条不同构造-岩浆杂岩带的形成构造环境:岩石学报,11(2):115-126.
    周鼎武,张成立,刘良,王居里,王焰,刘金平.2000.秦岭造山带及相邻地块元古代基性岩墙群研究综述及相关问题探讨.岩石学报,16(1):22-28.
    周鼎武,张成立.1994.论北秦岭加里东期造山作用.西北大学学报(自然科学版),24(3):245-250.
    周鼎武,张泽军,董云鹏,刘良.1995b.东秦岭商南松树沟元古宙蛇绿岩片的地质地球化学特征.岩石学报,11(增刊):154-164.
    周炼,高山,刘勇胜,凌文黎,张利.2007.扬子克拉通北缘碎屑沉积岩地球化学特征及意义.地球科学-中国地质大学学报,32(1):29-38.
    周艳艳,赵太平,薛良伟,王世炎,高剑峰.2009.河南嵩山地区新太古代TTG质片麻岩的成因及其地质意义:来自岩石学、地球化学及同位素年代学的制约.岩石学报,25(2):331-347.
    朱炳泉,常向阳,邱华宁,孙大中.1998.地球化学急变带的元古界基底特征及其与超大型矿床产出的关系.中国科学(D辑:地球科学),28(增刊):63-70.
    朱炳泉.1993.矿石Pb同位素三维空间拓扑图解用于地球化学省与矿种区划.地球化学,22(3):209-216.
    祝禧艳,陈福坤,王伟,王芳,张福勤.2008.豫西地区秦岭造山带武当群火山岩和沉积岩锆石U-Pb年龄.地球学报,29(6):817-829.
    祝禧艳,陈福坤,杨力,王伟,Trung, H. P.,苗来成,张福勤.2009.豫西地区秦岭造山带武当群Nd-Hf同位素组成及其物源特征.岩石学报,25(11):3017-3028.
    祝禧艳.2010.东秦岭造山带基底演化与属性:地球化学和年代学证据.博士论文:中国科学院地质与地球物理研究所,pp 1-138.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700