西天山卡特巴阿苏金铜矿区中性侵入岩地球化学特征及地质意义
|
摘要
卡特巴阿苏金铜矿矿区中性侵入岩研究表明,中性侵入岩的SiO_2含量较高,稀土元素整体表现为LREE富集,HREE亏损的分馏模式,微量元素总体显示出亏损Nb、Ta、Ti等高场强元素,富集Rb、Ce、Ba、Th等大离子亲石元素。三类中性侵入岩成因无明显的联系,为不同源成岩,属于晚石炭世混源序列,兼具原始地幔和岛弧火山岩的特征,岩石由遭受消减板片流体交代地幔源区部分熔融形成,兼具板内玄武岩和火山弧玄武岩的构造特征,为强烈的大陆裂谷伸展作用的产物。对全岩矿化闪长岩锆石U-Pb测试结果显示,闪长岩的侵位年龄为(305.0±2.0)Ma,为晚石炭世成岩,这与前人获得的载金黄铁矿(310.9±4.2)Ma的年龄在误差范围内一致,认为该矿床形成于造山后伸展环境之下,矿床深部可能存在与中性岩有关的斑岩型铜金矿体。
The study of neutral intrusive rocks in the Kateba'asu Au-Cu deposit ore mine shows that the content of SiO2 intrusive rocks is higher,and the REEs are characterized by LREE enrichment and fractional distillation of HREE loss.The trace elements generally show loss of high field strength elements such as Nb,Ta,and Ti,enriched in large ion lithophile elements such as Rb,Ce,Ba,and Th.There is no obvious relationship between the three types of neutral intrusive rocks,which are different source rocks and belong to the late Carboniferous mixed source sequence,which is characterized by both the original mantle and the island arc volcanic rocks.The rocks are partially melted by the reduction of the mantle source zone,both the structural characteristics of intraplate basalts and volcanic arc basalts are the products of strong continental rift extension.The zircon U-Pb test results of the whole rock mineralization diorite reveal that the emplacement age of the diorite is(305.0±2.0)Ma,which is the late Carboniferous diagenesis,which is similar to the previous gold-bearing pyrite(310.9 ± 4.2)Ma.The age is consistent within the error range.It is believed that the deposit is formed in the post-orogenic extension of the environment,and there may be associated with the Neoproterozoic porphyry copper-gold ore body.
The study of neutral intrusive rocks in the Kateba'asu Au-Cu deposit ore mine shows that the content of SiO2 intrusive rocks is higher,and the REEs are characterized by LREE enrichment and fractional distillation of HREE loss.The trace elements generally show loss of high field strength elements such as Nb,Ta,and Ti,enriched in large ion lithophile elements such as Rb,Ce,Ba,and Th.There is no obvious relationship between the three types of neutral intrusive rocks,which are different source rocks and belong to the late Carboniferous mixed source sequence,which is characterized by both the original mantle and the island arc volcanic rocks.The rocks are partially melted by the reduction of the mantle source zone,both the structural characteristics of intraplate basalts and volcanic arc basalts are the products of strong continental rift extension.The zircon U-Pb test results of the whole rock mineralization diorite reveal that the emplacement age of the diorite is(305.0±2.0)Ma,which is the late Carboniferous diagenesis,which is similar to the previous gold-bearing pyrite(310.9 ± 4.2)Ma.The age is consistent within the error range.It is believed that the deposit is formed in the post-orogenic extension of the environment,and there may be associated with the Neoproterozoic porphyry copper-gold ore body.
引文
[1]成守德.中国新疆北部及邻区贵重有色金属矿产成矿图说明书[M].北京:中国地质大学出版社,1996:97-106.Cheng Shoude.Metallogenic map of precious nonferrous metals in northern xinjiang and adjacent areas of China[M].Beijing:China University of Geosciences Press,1996:97-106.
[2]薛春纪,赵晓波,莫宣学,等.西天山巨型金铜铅锌成矿带构造成矿演化和找矿方向[J].地质学报,2014,88(12):2490-2531.XUE Chunji,ZHAO Xiaobo, MO Xuanxue,et al.Tectonic Metallogenic Evolution of Western Tianshan Giant Au-Cu-Zn-Pb Metallogenic Belt and Prospecting Orientation[J].Acta Geologica Sinica,2014,88(12):2490-2531.
[3]FRIMMEL H E.Earth's continental crustal gold endowment[J].Earth and Planetary Science Letters,2008,267(1):45-55.
[4]MAO Jinwen,KONOPELKO D,SELTMANN R,et al.Post collisional age of the Kumtor gold deposit and timing of Hercynian events in the Tien Shan,Kyrgyzstan[J].Economic Geology,2004,99(8):1771-1780.
[5]COOKE D R,HOLLINGS P,WALSHE J L.Giant porphyry deposits:characteristics,distribution,and tectonic controls[J].Economic Geology,2005,100(5):801-818.
[6]JENCHURAEVA R J.Tectonic settings of porphyrytype mineralization and hydrothermal alteration in Paleozoic island arcs and active continental margins,Kyrghyz Range,(Tien Shan)Kyrghyzstan[J].Mineralium Deposita,1997,32(5):434-440.
[7]薛春纪,赵晓波,莫宣学,等.西天山“亚洲金腰带”及其动力背景和成矿控制与找矿[J].地学前缘,2014,21(5):128-155.XUE Chunji,ZHAO Xiaobo,MO Xuanxue,et al.Asian Gold Belt in western Tianshan and its dynamic setting,metallogenic control exploration[J]. Earth Science Frontiers,2014,21(5):128-155.
[8]朱志新,王克卓,郑玉洁,等.新疆伊犁地块南缘志留纪和泥盆纪花岗质侵入体锆石SHRIMP定年及其形成时构造背景的初步探讨[J].岩石学报,2006,22(5):1193-1200.ZHU Zhixin,WANG Kezhuo,ZHENG Yujie,et al.Zircon SHRIMP dating of Silurian and Devonian granitic intrusions in the southern Yili block, Xinjiang and preliminary discussion on their tectonic setting[J].Acta Petrologica Sinica,2006,22(5):1193-1200.
[9]李锦轶,何国琦,徐新,等.新疆北部及邻区地壳构造格架及其形成过程的初步探讨[J].地质学报,2006,80(1):148-168.LI Jinyi,HE Guoqi,XU Xin,et al.Crustal Tectonic Framework of Northern Xinjiang and Adjacent Regions and Its Formation[J].Acta Geologica Sinica,2006,80(1):148-168.
[10]薛春纪,赵晓波,莫宣学,等.西天山巨型金铜铅锌成矿带构造成矿演化和找矿方向[J].地质学报,2014,88(12):2490-2531.XUE Chunji,ZHAO Xiaobo, MO Xuanxue,et al.Tectonic metallogenic evolution of Western Tianshan Giant Au-Cu-Zn-Pb metallogenic belt and prospecting orientation[J].Acta Geologica Sinica,2014,88(12):2490-2531.
[11]杨维忠,邢令,林泽华,等.新疆卡特巴阿苏金矿床特征及发现意义[J].新疆地质,2015,33(1):68-72.YANG Weizhong,XING Ling,LIN Zehua,et al.The characteristics and discovery significance of Kateba’asu gold deposit in Xinjiang[J].Xinjiang Geology,2015,33(1):68-72.
[12]李真,刘云华,王海涛,等.西天山卡特巴阿苏金铜矿床围岩蚀变特征及地质意义[J].新疆地质,2016,34(3):350-359.LI Zhen, LIU Yunhua, WANG Haitao, et al.Characteristics of Wall Rock Alteration and Geological Significance in Kateba'asu Au-Cu Deposit, Western Tianshan Mountains,Xinjiang[J].Xinjiang Geology,2016,34(3):350-359.
[13]刘云华,李真,莫宣学,等.西天山卡特巴阿苏矽卡岩型-破碎带蚀变岩型金铜矿床地质特征[J].吉林大学学报,2016,46(5):1368-1382.LIU Yunhua,LI Zhen,MO Xuanxue,et al.Geological characteristic of skarn-fracture zone altered rock type of the Kateba'asu Au-Cu Deposit in Western Tianshan Mountains in Xinjiang[J].Journal of Jilin University,2016,46(5):1368-1382.
[14]冯博,薛春纪,赵晓波,等.西天山卡特巴阿苏大型金铜矿赋矿二长花岗岩岩石学、元素组成和时代[J].地学前缘,2014,21(5):187-195.FENG Bo, XUE Chunji, ZHAO Xiaobo,et al.Petrology, geochemistry and zircon U-Pb isotope chronology of monzogranite of the Katbasu Au-Cu deposit,western Tianshan, Xinjiang Province[J].Earth Science Frontiers,2014,21(5):187-195.
[15]邢令,杨维忠,藏梅,等.新疆卡特巴阿苏金铜矿区二长花岗岩锆石SHRIMP U-Pb年龄及其地质意义[J].新疆地质,2015,33(1):1-6.XING Ling,YANG Weizhong,ZANG Mei,et al.Zircon SHRIMP U-Pb Dating of the Monzonitic granite from Kateba'asu Au-Cu deposit and its geological implications in Xinjiang[J].Xinjiang Geology,2015,33(1):1-6.
[16]张祺,薛春纪,赵晓波,等.新疆西天山卡特巴阿苏大型金矿床地质地球化学和成岩成矿年代[J].中国地质,2015,42(3):411-437.ZHANG Qi,XUE Chunji,ZHAO Xiaobo,et al.Geology,geochemistry and metallogenic epoch of the Kateba'asu large-sized gold deposit,Western Tianshan Mountains,Xinjiang[J].Geology in China,2015,42(3):411-437.
[17]高永伟,张振亮,王志华.等.西天山卡特巴阿苏金矿床成矿年代学及其地质意义-来自绢云母40 Ar-39 Ar同位素年龄证据[J].地质与勘探,2015,51(5):805-815.GAO Yongwei,ZHANG Zhenliang,WANG Zhihua,et al.Geochronology of the Kateba'asu gold deposit in West Tianshan and its geological significance evidence from40 Ar-39 Ar isotopic ages of sericite[J].Geology and Exploration,2015,51(5):805-815.
[18]邢令,藏梅,杨维忠,等.新疆卡特巴阿苏金铜矿全岩矿化小岩体的发现及其地质意义[J].新疆地质,2016,34(2):211-217.XING Ling,ZANG Mei,YANG Weizhong,et al.Discovery of the mineralization diorite in Kateba'asu gold-copper deposit, Xinjiang and its geological significance[J]. Xinjiang Geology,2016,34(2):211-217.
[19]李锦轶,王克卓,李亚平,等.天山山脉地貌特征、地壳组成与地质演化[J].地质通报,2006,25(8):895-909.LI Jinyi, WANG Kezhuo, LI Yaping, et al.Geomorphological features,crustal composition and geological evolution of the Tianshan Mountains[J].Geological Bulletin of China,2006,25(8):895-909.
[20]左国朝,张作衡,王志良,等.新疆西天山地区构造单元划分、地层系统及其构造演化[J].地质论评,2009,54(6):748-767.ZUO Guochao,ZHANG Zuoheng,WANG Zhiliang,et al.Tectonic division,stratigraphical system and the evolution of Western Tianshan Mountains,Xinjiang[J].Geological Review,2009,54(6):748-767.
[21]张良臣,吴乃元.天山地质构造及演化史[J].新疆地质,1985,3(3):1-14.ZHANG Liangchen,WU Naiyuan.The geotectonic and its evolution of TianShan[J].Xinjiang Geology,1985,3(3):1-14.
[22]杨维忠,薛春纪,赵晓波,等.新疆西天山新发现新源县卡特巴阿苏大型金铜矿床[J].吉林大学学报(地球科学版),2013,32(10):1613-1620.YANG Weizhong,XUE Chunji,ZHAO Xiaobo,et al.The discovery of the Kateba'asu large Au-Cu deposit in Xinyuan County, western Tianshan,Xinjiang[J].Geological Bulletin of China,2013,32(10):1613-1620.
[23]郭虎,王家松.用于同位素分析的锆石样品的系统制备方法[J].洛阳师范学院学报,2011,30(11):32-34.GUO Hu,WANG Jiasong.A systematic preparation of the Zircon sample in the determination of isotope[J].Journal of Luoyang Normal University,2011,30(11):32-34.
[24]ANDERSEN T.Correction of common lead in U-Pb analyses that do not report 204Pb[J].Chemical Geology,2002,192(1/2):59-79.
[25]LUDWIG K R.User’s manual for Isoplot 3.00:A Geochronologucal toolkit for Micosoft Excel[J].Berkeley Geochronology Center,Special Publication,2003,4:70.
[26]CHAPPELL B W,WHITE A J R.I-and S-type granites in the Lachlan Fold Belt[J].Geological Society of America Special Papers,1992,272:1-26.
[27]PECCERILLO R,TAYLOR S R.Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area,Northern Turkey[J].Contrib.Mineral Petrol,1976,58:63-84.
[28]MIDDLEMOST E A K.Naming materials in the magma/igneous rock system[J]. Earth Science Reviews,1994,37(3/4):215-224.
[29]SUN S S and MCDONOUGH W F.The Chemical and isotopic ystematics of oceanic basalts:Implications for mantle composition and process.In:Saunders AD and Norry MJ(eds).Magmatism in the Ocean Basins[J].Geological Society,London,Special Publication,1989,42(1):313-345.
[30]吴元保,郑永飞.锆石成因矿物学研究及其对U-Pb年龄解释的制约[J].科学通报,2004,49(16):1589.WU Yuanbao, ZHENG Yongfei. Zircon genetic mineralogy and its constraints on U-Pb age interpretation[J].Chinese Science Bulletin,2004,49(16):1589.
[31]BELOUSOVA E A,GRIFFIN W L O,REILLY S Y,et al.Igneous zircon:Trace element composition as an indicator of source rock type[J].Contributions to Mineralogy and Petrology,2002,143:602-622.
[32]FALLOON T J,GREEN D H,HATTON C J,et al.Anhydrous partial melting and depleted peridotite from2to 30kb and application to basalt petrogenesis[J].Journal of Petrology,1988,29(6):1257-1282.
[33]GREEN T H.Significance of Nb/Ta as an indicator of geochemical processes in the crust-mantle system[J].Chemical Geology,1995,120(3):347-359.
[34]刘永江,刘宾强,冯志强,等.大兴安岭中北段老道口闪长岩锆石U-Pb年龄、地球化学特征及构造意义[J].吉林大学学报(地球科学版),2016,46(2):482-498.LIU Yongjiang,LIU Binqiang,FENG Zhiqiang,et al.SIMS Gircon U-Pb age,pctrogcochcmistry and its tectonic implication of laodaokou diorite in the mid-north part of great xing'an range[J].Journal of Jilin University(Earth Science Edition),2016,46(2):482-498.
[35]IONOV D A,GRIFFIN W L,O′REILLY S Y.Volatile-bearing minerals and lithophile trace elements in the upper mantle[J].Chemical Geology,1997,141(3/4):153-184.
[36]MCDONOUGH W F,SUN S S.The Composition of the Earth[J].Chemical Geology,1995,120(3/4):223-253.
[37]金振民,高山.底侵作用(underplaiting)及其壳—幔演化动力学意义[J].地质科技情报,1996,25(2):1-7.JIN Zhenmin, GAO Shan. Underplating and its geodynamical significances for the evolution of crustmantle boundary[J].Geological Science and Technology Information,1996,25(2):1-7.
[38]高山,金振民.拆沉作用(delaminatiaon)及其壳—幔演化动力学意义[J].地质科技情报,1997,26(1):1-9.GAO Shan, JIN Zhenmin. Delamination and its geodynamical significance for the crust-mantle evolution[J].Geological Science and Technology Information,1997,26(1):1-9.
[39]朱志新,董连慧,王克卓,等.西天山造山带构造单元划分与构造演化[J].地质通报,2013,32(2/3):297-311.ZHU Zhixin,DONG Lianhui,WANG Kezhuo,et al.Tectonic division and regional tectonic evolution of West Tianshan organic belt[J].Geological Bulletin of China,2013,32(2/3):297-311.
[40]王洁明,赵文平,董苏庆.西天山那拉提构造—岩浆岩带石炭纪花岗岩岩石地球化学特征及侵位机制探讨[J].陕西地质,2010,28(2):47-52.WANG Jieming,ZHAO Wenping, DONG Suqing.Lithogeochemical features and emplacement of the carboniferous granite in the nalati structure-magmatite zone of western TianShan Mountain[J].Geology of ShaanXi,2010,28(2):47-52.
[41]WOOD D A.The application of Th-Hf-Ta diagram to problems of tectonomagmatic classification and to establishing the nature of crustal contamination of basalitic lavas of the British Tertiary volcanic province[J].Earth Plante.Sei.Lett,1980,50:11-30.
[42]MESEHEEDE M A.Method of discriminating between different types of mid-ocean ridge basalts and continental tholeiites with Nd-Zr-Y diagram[J].Chem.Geol,1986,56:207-218.
[43]汪云亮,张成江.玄武岩类形成的大地构造环境的Ta/Hf-Th/Hf图解判别[J].岩石学报,2001,17(3):414-418.WANG Yunliang,ZHANG Chengjiang.Ta/Hf-Th/Hf identification of tectonic setting of basalts[J].Acta Petrologica Sinica,2001,17(3):414-418.
[44]PASAVA J,VYMAZLOVA A,KOSLER J,et al.Platinum-group elements on ores from the Lalmakyr porphyry Cu-Au-Mo deposit, Uzbekistan; Bulk geochemical and laser Ablation ICPMS data[J].Mineralium Deposita,2010,100(5):801-818.
[2]薛春纪,赵晓波,莫宣学,等.西天山巨型金铜铅锌成矿带构造成矿演化和找矿方向[J].地质学报,2014,88(12):2490-2531.XUE Chunji,ZHAO Xiaobo, MO Xuanxue,et al.Tectonic Metallogenic Evolution of Western Tianshan Giant Au-Cu-Zn-Pb Metallogenic Belt and Prospecting Orientation[J].Acta Geologica Sinica,2014,88(12):2490-2531.
[3]FRIMMEL H E.Earth's continental crustal gold endowment[J].Earth and Planetary Science Letters,2008,267(1):45-55.
[4]MAO Jinwen,KONOPELKO D,SELTMANN R,et al.Post collisional age of the Kumtor gold deposit and timing of Hercynian events in the Tien Shan,Kyrgyzstan[J].Economic Geology,2004,99(8):1771-1780.
[5]COOKE D R,HOLLINGS P,WALSHE J L.Giant porphyry deposits:characteristics,distribution,and tectonic controls[J].Economic Geology,2005,100(5):801-818.
[6]JENCHURAEVA R J.Tectonic settings of porphyrytype mineralization and hydrothermal alteration in Paleozoic island arcs and active continental margins,Kyrghyz Range,(Tien Shan)Kyrghyzstan[J].Mineralium Deposita,1997,32(5):434-440.
[7]薛春纪,赵晓波,莫宣学,等.西天山“亚洲金腰带”及其动力背景和成矿控制与找矿[J].地学前缘,2014,21(5):128-155.XUE Chunji,ZHAO Xiaobo,MO Xuanxue,et al.Asian Gold Belt in western Tianshan and its dynamic setting,metallogenic control exploration[J]. Earth Science Frontiers,2014,21(5):128-155.
[8]朱志新,王克卓,郑玉洁,等.新疆伊犁地块南缘志留纪和泥盆纪花岗质侵入体锆石SHRIMP定年及其形成时构造背景的初步探讨[J].岩石学报,2006,22(5):1193-1200.ZHU Zhixin,WANG Kezhuo,ZHENG Yujie,et al.Zircon SHRIMP dating of Silurian and Devonian granitic intrusions in the southern Yili block, Xinjiang and preliminary discussion on their tectonic setting[J].Acta Petrologica Sinica,2006,22(5):1193-1200.
[9]李锦轶,何国琦,徐新,等.新疆北部及邻区地壳构造格架及其形成过程的初步探讨[J].地质学报,2006,80(1):148-168.LI Jinyi,HE Guoqi,XU Xin,et al.Crustal Tectonic Framework of Northern Xinjiang and Adjacent Regions and Its Formation[J].Acta Geologica Sinica,2006,80(1):148-168.
[10]薛春纪,赵晓波,莫宣学,等.西天山巨型金铜铅锌成矿带构造成矿演化和找矿方向[J].地质学报,2014,88(12):2490-2531.XUE Chunji,ZHAO Xiaobo, MO Xuanxue,et al.Tectonic metallogenic evolution of Western Tianshan Giant Au-Cu-Zn-Pb metallogenic belt and prospecting orientation[J].Acta Geologica Sinica,2014,88(12):2490-2531.
[11]杨维忠,邢令,林泽华,等.新疆卡特巴阿苏金矿床特征及发现意义[J].新疆地质,2015,33(1):68-72.YANG Weizhong,XING Ling,LIN Zehua,et al.The characteristics and discovery significance of Kateba’asu gold deposit in Xinjiang[J].Xinjiang Geology,2015,33(1):68-72.
[12]李真,刘云华,王海涛,等.西天山卡特巴阿苏金铜矿床围岩蚀变特征及地质意义[J].新疆地质,2016,34(3):350-359.LI Zhen, LIU Yunhua, WANG Haitao, et al.Characteristics of Wall Rock Alteration and Geological Significance in Kateba'asu Au-Cu Deposit, Western Tianshan Mountains,Xinjiang[J].Xinjiang Geology,2016,34(3):350-359.
[13]刘云华,李真,莫宣学,等.西天山卡特巴阿苏矽卡岩型-破碎带蚀变岩型金铜矿床地质特征[J].吉林大学学报,2016,46(5):1368-1382.LIU Yunhua,LI Zhen,MO Xuanxue,et al.Geological characteristic of skarn-fracture zone altered rock type of the Kateba'asu Au-Cu Deposit in Western Tianshan Mountains in Xinjiang[J].Journal of Jilin University,2016,46(5):1368-1382.
[14]冯博,薛春纪,赵晓波,等.西天山卡特巴阿苏大型金铜矿赋矿二长花岗岩岩石学、元素组成和时代[J].地学前缘,2014,21(5):187-195.FENG Bo, XUE Chunji, ZHAO Xiaobo,et al.Petrology, geochemistry and zircon U-Pb isotope chronology of monzogranite of the Katbasu Au-Cu deposit,western Tianshan, Xinjiang Province[J].Earth Science Frontiers,2014,21(5):187-195.
[15]邢令,杨维忠,藏梅,等.新疆卡特巴阿苏金铜矿区二长花岗岩锆石SHRIMP U-Pb年龄及其地质意义[J].新疆地质,2015,33(1):1-6.XING Ling,YANG Weizhong,ZANG Mei,et al.Zircon SHRIMP U-Pb Dating of the Monzonitic granite from Kateba'asu Au-Cu deposit and its geological implications in Xinjiang[J].Xinjiang Geology,2015,33(1):1-6.
[16]张祺,薛春纪,赵晓波,等.新疆西天山卡特巴阿苏大型金矿床地质地球化学和成岩成矿年代[J].中国地质,2015,42(3):411-437.ZHANG Qi,XUE Chunji,ZHAO Xiaobo,et al.Geology,geochemistry and metallogenic epoch of the Kateba'asu large-sized gold deposit,Western Tianshan Mountains,Xinjiang[J].Geology in China,2015,42(3):411-437.
[17]高永伟,张振亮,王志华.等.西天山卡特巴阿苏金矿床成矿年代学及其地质意义-来自绢云母40 Ar-39 Ar同位素年龄证据[J].地质与勘探,2015,51(5):805-815.GAO Yongwei,ZHANG Zhenliang,WANG Zhihua,et al.Geochronology of the Kateba'asu gold deposit in West Tianshan and its geological significance evidence from40 Ar-39 Ar isotopic ages of sericite[J].Geology and Exploration,2015,51(5):805-815.
[18]邢令,藏梅,杨维忠,等.新疆卡特巴阿苏金铜矿全岩矿化小岩体的发现及其地质意义[J].新疆地质,2016,34(2):211-217.XING Ling,ZANG Mei,YANG Weizhong,et al.Discovery of the mineralization diorite in Kateba'asu gold-copper deposit, Xinjiang and its geological significance[J]. Xinjiang Geology,2016,34(2):211-217.
[19]李锦轶,王克卓,李亚平,等.天山山脉地貌特征、地壳组成与地质演化[J].地质通报,2006,25(8):895-909.LI Jinyi, WANG Kezhuo, LI Yaping, et al.Geomorphological features,crustal composition and geological evolution of the Tianshan Mountains[J].Geological Bulletin of China,2006,25(8):895-909.
[20]左国朝,张作衡,王志良,等.新疆西天山地区构造单元划分、地层系统及其构造演化[J].地质论评,2009,54(6):748-767.ZUO Guochao,ZHANG Zuoheng,WANG Zhiliang,et al.Tectonic division,stratigraphical system and the evolution of Western Tianshan Mountains,Xinjiang[J].Geological Review,2009,54(6):748-767.
[21]张良臣,吴乃元.天山地质构造及演化史[J].新疆地质,1985,3(3):1-14.ZHANG Liangchen,WU Naiyuan.The geotectonic and its evolution of TianShan[J].Xinjiang Geology,1985,3(3):1-14.
[22]杨维忠,薛春纪,赵晓波,等.新疆西天山新发现新源县卡特巴阿苏大型金铜矿床[J].吉林大学学报(地球科学版),2013,32(10):1613-1620.YANG Weizhong,XUE Chunji,ZHAO Xiaobo,et al.The discovery of the Kateba'asu large Au-Cu deposit in Xinyuan County, western Tianshan,Xinjiang[J].Geological Bulletin of China,2013,32(10):1613-1620.
[23]郭虎,王家松.用于同位素分析的锆石样品的系统制备方法[J].洛阳师范学院学报,2011,30(11):32-34.GUO Hu,WANG Jiasong.A systematic preparation of the Zircon sample in the determination of isotope[J].Journal of Luoyang Normal University,2011,30(11):32-34.
[24]ANDERSEN T.Correction of common lead in U-Pb analyses that do not report 204Pb[J].Chemical Geology,2002,192(1/2):59-79.
[25]LUDWIG K R.User’s manual for Isoplot 3.00:A Geochronologucal toolkit for Micosoft Excel[J].Berkeley Geochronology Center,Special Publication,2003,4:70.
[26]CHAPPELL B W,WHITE A J R.I-and S-type granites in the Lachlan Fold Belt[J].Geological Society of America Special Papers,1992,272:1-26.
[27]PECCERILLO R,TAYLOR S R.Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area,Northern Turkey[J].Contrib.Mineral Petrol,1976,58:63-84.
[28]MIDDLEMOST E A K.Naming materials in the magma/igneous rock system[J]. Earth Science Reviews,1994,37(3/4):215-224.
[29]SUN S S and MCDONOUGH W F.The Chemical and isotopic ystematics of oceanic basalts:Implications for mantle composition and process.In:Saunders AD and Norry MJ(eds).Magmatism in the Ocean Basins[J].Geological Society,London,Special Publication,1989,42(1):313-345.
[30]吴元保,郑永飞.锆石成因矿物学研究及其对U-Pb年龄解释的制约[J].科学通报,2004,49(16):1589.WU Yuanbao, ZHENG Yongfei. Zircon genetic mineralogy and its constraints on U-Pb age interpretation[J].Chinese Science Bulletin,2004,49(16):1589.
[31]BELOUSOVA E A,GRIFFIN W L O,REILLY S Y,et al.Igneous zircon:Trace element composition as an indicator of source rock type[J].Contributions to Mineralogy and Petrology,2002,143:602-622.
[32]FALLOON T J,GREEN D H,HATTON C J,et al.Anhydrous partial melting and depleted peridotite from2to 30kb and application to basalt petrogenesis[J].Journal of Petrology,1988,29(6):1257-1282.
[33]GREEN T H.Significance of Nb/Ta as an indicator of geochemical processes in the crust-mantle system[J].Chemical Geology,1995,120(3):347-359.
[34]刘永江,刘宾强,冯志强,等.大兴安岭中北段老道口闪长岩锆石U-Pb年龄、地球化学特征及构造意义[J].吉林大学学报(地球科学版),2016,46(2):482-498.LIU Yongjiang,LIU Binqiang,FENG Zhiqiang,et al.SIMS Gircon U-Pb age,pctrogcochcmistry and its tectonic implication of laodaokou diorite in the mid-north part of great xing'an range[J].Journal of Jilin University(Earth Science Edition),2016,46(2):482-498.
[35]IONOV D A,GRIFFIN W L,O′REILLY S Y.Volatile-bearing minerals and lithophile trace elements in the upper mantle[J].Chemical Geology,1997,141(3/4):153-184.
[36]MCDONOUGH W F,SUN S S.The Composition of the Earth[J].Chemical Geology,1995,120(3/4):223-253.
[37]金振民,高山.底侵作用(underplaiting)及其壳—幔演化动力学意义[J].地质科技情报,1996,25(2):1-7.JIN Zhenmin, GAO Shan. Underplating and its geodynamical significances for the evolution of crustmantle boundary[J].Geological Science and Technology Information,1996,25(2):1-7.
[38]高山,金振民.拆沉作用(delaminatiaon)及其壳—幔演化动力学意义[J].地质科技情报,1997,26(1):1-9.GAO Shan, JIN Zhenmin. Delamination and its geodynamical significance for the crust-mantle evolution[J].Geological Science and Technology Information,1997,26(1):1-9.
[39]朱志新,董连慧,王克卓,等.西天山造山带构造单元划分与构造演化[J].地质通报,2013,32(2/3):297-311.ZHU Zhixin,DONG Lianhui,WANG Kezhuo,et al.Tectonic division and regional tectonic evolution of West Tianshan organic belt[J].Geological Bulletin of China,2013,32(2/3):297-311.
[40]王洁明,赵文平,董苏庆.西天山那拉提构造—岩浆岩带石炭纪花岗岩岩石地球化学特征及侵位机制探讨[J].陕西地质,2010,28(2):47-52.WANG Jieming,ZHAO Wenping, DONG Suqing.Lithogeochemical features and emplacement of the carboniferous granite in the nalati structure-magmatite zone of western TianShan Mountain[J].Geology of ShaanXi,2010,28(2):47-52.
[41]WOOD D A.The application of Th-Hf-Ta diagram to problems of tectonomagmatic classification and to establishing the nature of crustal contamination of basalitic lavas of the British Tertiary volcanic province[J].Earth Plante.Sei.Lett,1980,50:11-30.
[42]MESEHEEDE M A.Method of discriminating between different types of mid-ocean ridge basalts and continental tholeiites with Nd-Zr-Y diagram[J].Chem.Geol,1986,56:207-218.
[43]汪云亮,张成江.玄武岩类形成的大地构造环境的Ta/Hf-Th/Hf图解判别[J].岩石学报,2001,17(3):414-418.WANG Yunliang,ZHANG Chengjiang.Ta/Hf-Th/Hf identification of tectonic setting of basalts[J].Acta Petrologica Sinica,2001,17(3):414-418.
[44]PASAVA J,VYMAZLOVA A,KOSLER J,et al.Platinum-group elements on ores from the Lalmakyr porphyry Cu-Au-Mo deposit, Uzbekistan; Bulk geochemical and laser Ablation ICPMS data[J].Mineralium Deposita,2010,100(5):801-818.
© 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 |