东宁地区早中生代花岗岩地球化学特征及大地构造背景
摘要
本文运用LA-ICPMS、ICPMS等先进实验测试技术对东宁地区花岗岩进行了年代学和地球化学研究,结合前人研究成果,对东宁-延边地区花岗岩的形成时代、地球化学特征、成因和大地构造背景等方面进行讨论,取得了一些认识。
东宁-延边地区花岗岩(包括太平岭、七十二顶子、闹枝沟和大荒沟等岩体)形成时代为晚三叠世(214-200Ma),岩石组合为花岗闪长岩-二长花岗岩,还有少量的石英闪长岩和钾长花岗岩,属于中钾钙碱性岩石系列,并有向高钾钙碱性演化的趋势。岩石学、岩石地球化学特征具有与大洋板块俯冲作用有关的科迪勒拉花岗岩的特征,反映在晚三叠世末期东宁-延边地区为一活动大陆边缘。
结合区域研究成果,本文得出东宁-延边地区晚三叠世花岗岩为滨太平洋构造域开始的标志,是古太平洋板块在晚三叠世对东北地区发生俯冲作用构造背景下的产物。
Dongning area, which is located within the eastern part of Heilongjiang province and the most eastern part of the Central Asian Orogenic Belt, form the southwestern continent margine of Khanka block with Yanbian area in Jinlin province and Russian Primorye, and develop geologic unit since late Paleozoic mainly. In the investigate region, immense volumes of granitic rocks emplaced during the Phanerozoic. This paper made a precise dating for the granodiorite of Taiping range pluton in the area, by U-Pb isotopic dating on zircon, and obtain 201±1Ma, which represent the age of the intrusion of this plutons. The age of Taiping range pluton is consistent with the ages of the 199±8Ma/206±4Ma of Qishierdingzi pluton, the 203±2/201±10Ma of Dahuanggou pluton and the 214±10Ma of Naozhigou Pluton. The new chronology framework of plutons in Dongning-Yanbian area has changed the previous viewpoint that all of these plutons formed during Late Permian-Early Triassic and reflect a magmatothermal event in the Dongning-Yanbian area at the end of late Triassic.
This paper research the petrological and geochemical characters amply on the Taiping range pluton and Qishierdingzi pluton. Combined with the previous datums on Naozhigou pluton and Dahuangou pluton, the late Triassic granites in Dongning-Yanbian are mainly composed of granodiorite and monzogranite, and some quartz diorite and K-feldspar granite. These granitoid rocks are hypidiomo- rphic granular or prophyaceous texture and massive structure. Many mafic magma enclaves are contained in the granite, and the characters of the shape, the texture, the minerals of the enclaves reflect the granitic magma is formed by mixing of high temperature basic magma and relative low temperature felsic magma. The petrologic geochemistry characters show these granites rich in CaO and Na2O, their Rittmann index(δ)=0.77- 2.78, < 3, A/CNK range from 0.84 to 1.25, most are less than 1.1,and ANK are more than 1, so all they are calc-alkaline metaluminous granites. These granites belong to medium K calc-alkaline series, and have a tendence that evolving into high-K calc-alkaline series, all they belong to I-typed granite. The primary mantle normalized spider diagrams of trace elements shows that these granites are rich in LILE (Rb, Th, K, La et al.), and the enrichment become more and more obvious with the evolvement of magmas, deplete Sr, P, Ti and the HFSE (Nb, Ta, Zr, Hf et al.) relatively, Ba show a slightly depletion compared with Rb and Th. Combined with the variety of main elements, the trace elements and REE variation indicate that the granitic magma has occurred fractional crystallisation during the magmatic evolution. The fractionating phase are hornblende and biotite during the early stage, and is plagioclase in the late stage, and some accessoy minerals (apatite and/or titanite) occurred fractional crystalli- zation also. The isotopic characters of low Isr and highεNd(t) of granites are similar with Phanerozoic granites in CAOB, and someone’s Isr are close to the Isr of ocean tholeiite, which indicate the contribution of oceanic crust to the formation of granitic magma. Through the comparation on petrologic, mineral assemble and geochemistry, these granites are similar with the ACG(ATG) and parts of KCG, which are eatablished by Barbarin(1999) and their formation are related to the subduction of oceanic crust. Using the tectonic discrimination diagram to judge the setting of the granites formation, all samples of the studied plutons fall within the field pre-plate collision and syn-collision granite of R1-R2 diagram (Batchelor et al.,1985), which show these granites have a relation with the subduction of oceanic crust.
The research on stratigraphy and paleontology, paleomagnetic, petrology and tectonic indicate that the paleo-Asian ocean closed along the west Lamulun river- Changchun- Yanji and the south block and north block have occurred intense convergence at the end of Permian. It become a integer at late Triassic.
The medium K cale-alkaline granite that form at the active continental margin at Late Triassic in Dongning-Yanbian and the early Jurassic high K calc-alkaline granite in Zhangguangcai range, which form at post-collision uplift set, form a changing tendence of composition. It reflect that there is a subduction of oceanic crust to the Northeast China at that time. It show that the paleo-Pacific plate has started to subduct under the Northeast China at the end of late Triassic.
东宁-延边地区花岗岩(包括太平岭、七十二顶子、闹枝沟和大荒沟等岩体)形成时代为晚三叠世(214-200Ma),岩石组合为花岗闪长岩-二长花岗岩,还有少量的石英闪长岩和钾长花岗岩,属于中钾钙碱性岩石系列,并有向高钾钙碱性演化的趋势。岩石学、岩石地球化学特征具有与大洋板块俯冲作用有关的科迪勒拉花岗岩的特征,反映在晚三叠世末期东宁-延边地区为一活动大陆边缘。
结合区域研究成果,本文得出东宁-延边地区晚三叠世花岗岩为滨太平洋构造域开始的标志,是古太平洋板块在晚三叠世对东北地区发生俯冲作用构造背景下的产物。
Dongning area, which is located within the eastern part of Heilongjiang province and the most eastern part of the Central Asian Orogenic Belt, form the southwestern continent margine of Khanka block with Yanbian area in Jinlin province and Russian Primorye, and develop geologic unit since late Paleozoic mainly. In the investigate region, immense volumes of granitic rocks emplaced during the Phanerozoic. This paper made a precise dating for the granodiorite of Taiping range pluton in the area, by U-Pb isotopic dating on zircon, and obtain 201±1Ma, which represent the age of the intrusion of this plutons. The age of Taiping range pluton is consistent with the ages of the 199±8Ma/206±4Ma of Qishierdingzi pluton, the 203±2/201±10Ma of Dahuanggou pluton and the 214±10Ma of Naozhigou Pluton. The new chronology framework of plutons in Dongning-Yanbian area has changed the previous viewpoint that all of these plutons formed during Late Permian-Early Triassic and reflect a magmatothermal event in the Dongning-Yanbian area at the end of late Triassic.
This paper research the petrological and geochemical characters amply on the Taiping range pluton and Qishierdingzi pluton. Combined with the previous datums on Naozhigou pluton and Dahuangou pluton, the late Triassic granites in Dongning-Yanbian are mainly composed of granodiorite and monzogranite, and some quartz diorite and K-feldspar granite. These granitoid rocks are hypidiomo- rphic granular or prophyaceous texture and massive structure. Many mafic magma enclaves are contained in the granite, and the characters of the shape, the texture, the minerals of the enclaves reflect the granitic magma is formed by mixing of high temperature basic magma and relative low temperature felsic magma. The petrologic geochemistry characters show these granites rich in CaO and Na2O, their Rittmann index(δ)=0.77- 2.78, < 3, A/CNK range from 0.84 to 1.25, most are less than 1.1,and ANK are more than 1, so all they are calc-alkaline metaluminous granites. These granites belong to medium K calc-alkaline series, and have a tendence that evolving into high-K calc-alkaline series, all they belong to I-typed granite. The primary mantle normalized spider diagrams of trace elements shows that these granites are rich in LILE (Rb, Th, K, La et al.), and the enrichment become more and more obvious with the evolvement of magmas, deplete Sr, P, Ti and the HFSE (Nb, Ta, Zr, Hf et al.) relatively, Ba show a slightly depletion compared with Rb and Th. Combined with the variety of main elements, the trace elements and REE variation indicate that the granitic magma has occurred fractional crystallisation during the magmatic evolution. The fractionating phase are hornblende and biotite during the early stage, and is plagioclase in the late stage, and some accessoy minerals (apatite and/or titanite) occurred fractional crystalli- zation also. The isotopic characters of low Isr and highεNd(t) of granites are similar with Phanerozoic granites in CAOB, and someone’s Isr are close to the Isr of ocean tholeiite, which indicate the contribution of oceanic crust to the formation of granitic magma. Through the comparation on petrologic, mineral assemble and geochemistry, these granites are similar with the ACG(ATG) and parts of KCG, which are eatablished by Barbarin(1999) and their formation are related to the subduction of oceanic crust. Using the tectonic discrimination diagram to judge the setting of the granites formation, all samples of the studied plutons fall within the field pre-plate collision and syn-collision granite of R1-R2 diagram (Batchelor et al.,1985), which show these granites have a relation with the subduction of oceanic crust.
The research on stratigraphy and paleontology, paleomagnetic, petrology and tectonic indicate that the paleo-Asian ocean closed along the west Lamulun river- Changchun- Yanji and the south block and north block have occurred intense convergence at the end of Permian. It become a integer at late Triassic.
The medium K cale-alkaline granite that form at the active continental margin at Late Triassic in Dongning-Yanbian and the early Jurassic high K calc-alkaline granite in Zhangguangcai range, which form at post-collision uplift set, form a changing tendence of composition. It reflect that there is a subduction of oceanic crust to the Northeast China at that time. It show that the paleo-Pacific plate has started to subduct under the Northeast China at the end of late Triassic.
引文
迟效国,戚长谋,齐永恒. 中国东部花岗岩荷载微粒闪长质包体成因.长春地质学院院刊,1995.25(2):131-143
崔革等.黑龙江省东部晚石炭-晚白垩世地层的古地磁特征及其地质意义.黑龙江地质,1991.(2) .
邓晋福,刘厚祥,赵海玲等. 燕辽地区燕山期火成岩与造山模型.现代地质,1996,10(02): 137-148
方文昌. 吉林省花岗岩类及成矿作用. 吉林科学技术出版社,1992,1-271
苑凤华,路孝平,乔国华.黑龙江省东南部闹枝沟岩体岩浆混合作用的野外地质学证据.吉林地质,2002,21(1-2)
葛文春,吴福元,周长勇等. 大兴安岭北部塔河花岗岩体的时代及对额尔古纳地块构造归属的制约. 科学通报,2005a, 50(12): 1239-1247
葛文春,吴福元,周长勇等. 大兴安岭中部乌兰浩特地区中生代花岗岩的锆石 U-Pb 年龄及地质意义. 岩石学报,2005b, 21(3): 749-762
黑龙江地矿局. 区域地质调查报告(穆棱镇公社幅和东宁县幅部分).1979.78-103
黑龙江地矿局. 黑龙江省区域地质志.北京:地质出版社,1993,347-418
洪大卫,王式桄,谢锡林等. 兴蒙造山带正 ε(Nd,t )值花岗岩的成因和大陆地壳生长.地学前缘,2000.7(2): 441-456
洪大卫,王式桄,谢锡林等. 从中亚正εNd值花岗岩看超大陆演化和大陆地壳生长的关系.地球学报,2003.77(2):203-209
黄宝春,朱鸿,谭承泽.吉林省东部地区古地磁结果的大地构造意义.地球物理学报,1994.37(增 1):304-315
贾大成. 延吉地体地质特征及构造演化探讨.吉林地质,1995.14(1):40-45
姜开君,周永昶. 吉林珲春地区大荒沟花岗岩岩基的岩浆演化和构造环境.地质论评,1993.39(5):465-475
李之彤,赵春荆. 东北地区的印支运动.地质科学,1985.3:211-223
李之彤,赵春荆. 吉黑东部晚三叠世岩浆岩活动及其与板块构造的关系.中国地质科学院院报,1988.18:21-32
李之彤,朱群. 吉黑东部花岗岩类的稳定同位素组成.岩石矿物学杂志,2001.20 (3):253-259
李锦轶,牛宝贵,宋彪等. 长白山北段地壳的形成与演化.北京:地质出版社,1999.1-137
李双林, 欧阳自远. 兴蒙造山带及邻区的构造格局与构造演化. 海洋地质与第四纪地质, 1998, 18(3): 45-54
李昌年. 火成岩微量元素岩石学.中国地质大学出版社,1992,1pp
李兆鼐等.中国东部中、新生代火成岩及其深部过程.北京:地质出版社,2003,70-75。
刘红涛,翟明国,刘建明等. 华北克拉通北缘中生代花岗岩: 从碰撞后到非造山. 岩石学报2002,18(4):433-448
刘伟,杨进辉,李潮峰. 内蒙赤峰地区若干主干断裂带的构造热年代学. 岩石学报,2003,19(4):717-728
刘先文. 吉林东部若干地质问题讨论.吉林地质科技情报,1994,17-19
刘建峰. 小兴安岭早古生代花岗岩地球化学特征及其构造意义.吉林大学硕士学位论文,2006.
路孝平,吴福元,赵成弼等. 通化地区印支期花岗岩锆石U-Pb年龄及其与大别苏鲁超高压带碰撞造山作用之间的关系.科学通报,2003,48(8):843-849
内蒙古地矿局.内蒙古区域地质志,北京:地质出版社,1991
彭玉鲸,王明胜. 走滑断裂带的两类花岗岩.吉林地质,1998,17(2):22-30
彭玉鲸,刘爱,李文锁等. 吉林省延边地区二叠纪的三类植物群与古陆缘再造.吉林地质,1999,18(1):1-12
裴福萍. 延边地区晚三叠世火山岩的岩石地球化学特征及其构造意义.世界地质,2004,23(1):6-13
齐成栋,纪春华,韩江等.吉林至珲春地区晚二叠世—早三叠世花岗岩成因机制.吉林地质,2005.24 (2):10-15
秦克章,田中亮吏,李伟实,石原舜三.满洲里地区印支期花岗岩Rb-Sr等时线年代学证据,岩石矿物学杂志,199 8 .17(3):235-240
任纪舜,陈延愚,牛宝贵等. 中国东部及邻区大陆岩石圈的构造演化与成矿. 北京: 科学出版社,1990
邵济安,唐克东,詹立培等. 一个古大陆边缘的再造及其大地构造意义——延边地质延吉新进展.中国科学(B 辑).1995.25(5):548-555
石玉若等. 内蒙古苏左旗地区闪长-花岗岩类 SHRIMP 年代学.地质学报,2004.78(6):789-799
史长义,鄢明才,刘崇民等. 中国花岗岩类化学元素丰度及特征.地球化学,2005,34(5):471-782
宋彪, 李锦轶, 牛宝贵等. 黑龙江省东部麻山群黑云斜长片麻岩中锆石的年龄及其地质意义. 地球学报, 1997, 18(3): 306-312
孙革.中国吉林天桥岭晚三叠世植物群.吉林科学技术出版社.1993.1-157
隋振民,葛文春,吴福元等.大兴安岭东北部哈拉巴奇花岗岩体锆石 U- Pb 年龄及其成因.世界地质.2006.25(3):229-236
孙德有,吴福元,李惠民等. 小兴安岭西北部造山后 A 型花岗岩的时代及与索伦山-贺根山-扎赉特碰撞拼合带东延的关系. 科学通报, 2000, 45 (20): 2217-2222
孙德有.张广才岭中生代花岗岩成因及其地球动力学意义. 吉林大学博士学位论文,2001
孙德有,吴福元,张艳斌等. 西拉木伦河-长春-延吉板块缝合带的最后闭合时间—来自吉林大玉山花岗岩体的证据.吉林大学学报(地球科学版),2004,34(2):174-181.
孙德有,吴福元,高山等. 吉林中部晚三叠世和早侏罗世两期铝质 A 型花岗岩的厘定及对吉黑东部构造格局的制约.地学前缘,2005,12(2):263-275
孙德有,吴福元,高山. 小兴安岭东部清水岩体的锆石激光探针 U-Pb 年龄测定.地球学报,2004,25(2):213-218
陶继雄,胡凤翔,陈志勇. 华北陆块北缘印支期S型花岗岩带特征及其构造环境.岩石矿物学杂志,2003,22(2):212-218
陶奎元,毛建仁,杨祝良等. 中国东南部中生代岩石构造组合和复合动力学过程的记录. 地学前缘, 1998, 5(4): 183-190
唐克东,王莹,何国琦等. 中国东北及邻区大陆边缘构造. 地质学报,1995,69(1):16-30
唐克东,邵济安,李景春等. 吉林延边缝合带的性质与东亚构造,地质通报,2004,23(9-10):885-891
吴福元,杨进辉,柳小明. 辽东半岛中生代花岗质岩浆作用的年代学格架. 高校地质学报, 2005,11(3):305-317
吴福元, 江博明, 林强. 中国北方造山带造山后花岗岩的同位素特点与地壳生长意义. 科学通报,1997, 42(20): 2188-2192
吴福元,林强,葛文春等.张广才岭新华屯岩体的形成时代与成因研究. 岩石矿物学杂志, 1998,17(3):226-234
吴福元, SWILDE, 孙德有. 佳木斯地块片麻状花岗岩的锆石离子探针 U-Pb 年龄. 岩石学报, 2001, 17(3): 443-452
吴福元,曹林. 东北亚地区的若干重要基础地质问题. 世界地质, 1999, 18(2): 1-13
吴福元,孙德有,林强. 东北地区显生宙花岗岩成因与地壳增生. 岩石学报,1999,15 (2) : 181-189
王五力,郑少林等.中国东北环太平洋带构造地层学.北京:地质出版社,1995. 160
王友勤. 关于中国东北区地层区划的意见. 吉林地质, 1996.15(3-4): 15-22
王友勤,张德英. 黑龙江省东南部陆相上三叠统德发现.地层学杂志,1984,8(4):308-313
王友勤,殷场健,赵春荆等. 黑龙江省东宁县闹枝沟印支期花岗岩体的发现及其地质意义.中国地质科学院沈阳地矿所所刊,1983.6:57-66
王占福. 延边地区前中生代主要变质岩地质演化特征概述.吉林地质.1998.17(2):31-41
王万军,孙振家,胡祥昭. 内蒙古前进场花岗岩体的地质特征及其构造环境.地质与勘探, 2005,44(2):35-40
王涛. 花岗岩混合成因研究及大陆动力学意义.岩石学报,2000a.16(02):161-168
王涛. 花岗岩研究与大陆动力学.地学前缘,2000b.7(增刊):137-146
武广,孙丰月,赵财胜等. 额尔古纳地块北缘早古生代后碰撞花岗岩的发现及其地质意义. 科学通报,2005,50(20): 2278-2288
杨金中,邱海峻,孙家鹏等. 跃进山岩系及其构造意义. 长春科技大学学报,1998,28:380-385
袁洪林,吴福元,高山等.东北地区新生代侵入体的锆石激光探针 U-Pb 年龄测定与稀土元素成分分析.科学通报,2003,48(14):1511-1520
张兴洲,杨宝俊,吴福元等.中国兴蒙-吉黑地区岩石圈结构基本特征.中国地质.2006.33(4):817-823
张艳斌,吴福元,孙德有等. 延边”早海西期”棉田花岗岩和仲坪紫苏辉石闪长岩的单颗粒锆石 U-Pb 定年.地质论评,2002a,48(4):224-229
张艳斌,吴福元,李惠民等. 吉林黄泥岭花岗岩体的单颗粒锆石 U-Pb 年龄,岩石学报, 2002b ,18 (4) : 475 – 481
张艳斌. 延边地区花岗质岩浆活动的同位素地质年代学格架. 吉林大学博士学位论文,2002c
张艳斌,吴福元,翟明国等. 和龙地块的构造属性与华北地台北缘东段边界.中国科学 D辑,2004,34(9):795-806.
张用焕,彭玉鲸,欧祥喜. 关于吉林省延边地区二叠纪的思考.吉林地质,2000.19(1):1-12
赵成弼,靳克,齐成栋等. 珲春地区早印支期I-A型花岗岩系的特征及其大地构造意义.吉林地质,2001.21(1):1-11
周建波,刘建辉,郑常青等. 大别-苏鲁造山带的东延及板块缝合线:郯庐-鸭绿江-延吉断裂的厘定.高校地质学报,2005.11(1):92-104
Andersen T. Correction of common lead in U-Pb analyses that do not resport 204Pb. Chem.Geol., 2002(192):59-79
Batchelor, B., Bowden, P.. Petrogenetic interpretation of granitoid rock series using multicationic parameters. Chemical Geology, 1985. 48:43–55.
Barbarin, B.. Granitoids: main petrogenetic classifications in relation to origin and tectonic setting. Geol. J, 1990.25, 227–238.
Barbarin,B. A review of the relationships between granitoid types, their origins and their geodynamic environments. Lithos,1999.46:605–626
Barth A.P., Wooden J.L., Tosda R.M. and Morrison,J. Crustal contamination in the petrogenesis of a calc-alkalic rock series:Josephine Mountain intrusion, Califo rnia. GSA Bulletin, 1995. 107(2) : 201- 212
Bartholomew, D.S., Tarney, J. Geochemical characteristics of magmatism in the southern Andes 45–46°S . Andean magmatism:chemical and isotopic constraints,1984.In: Harmon, R.S., Barreiro, B.A. Eds. , Shiva Publ., Nantwich, pp. 220-229.
Bateman, P.C., A summary of critical relations in the central part of the Sierra Nevada Batholith California, USA.Geol. Soc. Am. Mem,1983.159:241–254.
Bateman, P.C. Plutonism in the central part of the Sierra Nevada Batholith, California. US Geol. Surv. Prof,1992.Paper 1483:1–186
Boriani A.Origoni E.G and Pinarell L. Paleozoic evolution of southern Alpine crust (northern Italy ) as indicated by constrasting granitoid suites. Lithos,1995.35: 47～ 63
Castro A. H-type (Hybrid) granitoids: aproposed revision of the granite type classification and nomenclature. Earth Science Reviews, 1991. 31: 237～ 253
CollinsW J. S-and I-type granites of the eastern Lachlan fold belt: products of tree- component mixing. Transaction of the Royal Society of Edinburgh, Earth Sciences, 1996. 88: 171-179
Collins W J. Evaluation of petrogenetic models for Lachlan Fold Belt granitoids: implications for crustal architecture and tectonic models. Australian Journal of Sciences, 1998. 45: 483～ 500
Desouky M.D., Feely M. and Mortr P. Diorite-granite magma mingling and mixing along the axis of Galway Granite batholith,Ireland. Journal of the Society London, 1996. 153: 361-374
Faure M,Lin W,Le Breton N.Where is the North China-South China block boundary in eastern China? Geology,2001. 29: 119-122
Jahn, B.M., Wu, F.Y., Hong, D.W., Important crustal growth in the Phanerozoic: isotopic evidence of granitoids from East- central Asia.Proc. Indian Acad. Sci., Earth Planet. Sci., 2000a.109, 5-20.
Jahn, B.M., Wu, F.Y., Chen, B.,. Granitoids of the Central Asian Orogenic Belt and continental growth in the Phanerozoic. Trans. R. Soc. Edinb.: Earth Sci. ,2000c. 91, 181- 193.
Keay S, CollinsW J and Mc Culloch M T. A three-component mixing model for granitoid genesis: Lachlan Fold Belt, eastern Australia. Geology, 1997. 25: 307～310
Kovalenko, V.I., Yarmolyuk, V.V., Kovach, V.P., Kotov, A.B., Kozakov,I.K., Sal’nikova, E.B., 1996. Sources of Phanerozoic granitoids in Central Asia: Sm–Nd isotope data. Geochem.Int. 34, 628– 640.
M. Arslan, Z. Aslan.Mineralogy, petrography and whole-rock geochemistry of the Tertiary granitic intrusions in the Eastern Pontides, Turkey, Journal of Asian Earth Sciences ,2006.27 :177–193
Maruyama S. Pacific-type orogeny revisited: Miyashiro-type orogeny proposed. The Island Arc, 1997, 6: 91-120
Pearce, J.A., Harris, N.B.W., Tindle, A.G.. Trace element discrimination diagrams for the tectonic interpretation ofgranitic rocks. J. Petrol , 1984 .25, 956–983.
Pitcher, W.S... Granite Type and Tectonic Environment. In: Hsu, K. Ed. , Mountain Building Processes, Academic Press,London ,1983 .pp. 19–40.
Pitcher, W.S., Granites and yet more granites forty years on.Geol. Rundschau 1987. 76, 51–79.
Pitcher, W.S., The Nature and Origin of Granite. Blackie Acad. and Prof. ed., London, 1993.
Pitcher,W.S. The Nature and Origin of Granite. London:Chapman and Hall. 1997.
Soesoo A , Bons P D and Gray D R. Divergent double subduction: Tectonic and petrology consequences. Geology, 1997. 25: 755～758
Simon A. Wilde.Late Pan-African magmatism in northeastern China: SHRIMP U–Pb zircon evidence from granitoids in the Jiamusi Massif.Precambrian Research.2003.122 (2003) 311–327
Wilde, S.A., Wu, F.Y., Zhang, X.Z., The Mashan Complex:SHRIMP U–Pb zircon evidence for a Late Pan-Africanmetamorphic event in NE China and its implications for global continental reconstructions. Geochimica ,2001.30, 35–50 (in Chinese, with English abstract).}
Wiedenbeck M, Alle P, Corfu F et al. Three natural zircon standards for U-Th-Pb, Lu-Hf, trace element and REE analyses. Geostand Newsl, 1995(19): 1-23
Wu, F.-Y. et al..A-type granites in northeastern China:age and geochemical constraints on their petrogenesis, Chemical Geology ,2002.187,143-173
Wu, F.-Y. et al. Highly fractionated I-type granites in NE China(Ⅰ ): geochronology and petrogenesis. Lithos, 2003.66:241- 273
Wu, F.-Y. et al. Highly fractionated I-type granites in NE China(Ⅱ ):isotopic geochemistry and implications for crustal growth in the Phanerozoic.Lithos,2003 .67:191– 204
Wu, F.-Y. et al., The Hulan Group: Its role in the evolution of the Central Asian Orogenic Belt of NE China, Journal of Asian Earth Sciences (2007), doi:10.1016/j. jseaes.2007.01.003
Wu, F.-Y. et al. Initial constraints on the timing of granitic magmatism in North Korea using U–Pb zircon geochronology. Chem. Geol. 2007,doi:10.1016/j.chemgeo .2006.11.012
Yoji Arakawa.Two types of granitic intrusions in the Hida belt,Japan:Sr isotopic and chemical characteristics of the Mesozoic Funatsu granitic rocks.Chemical Geology, 1990.85:101-117.
Yoji Arakawa, Taro Shinmura.Nd-Sr isotopic and geochemical characteristics of two contrasting types of calc-alkaline plutons in the Hida belt,Japan,Chemical Geology, 1995.124: 217-232
崔革等.黑龙江省东部晚石炭-晚白垩世地层的古地磁特征及其地质意义.黑龙江地质,1991.(2) .
邓晋福,刘厚祥,赵海玲等. 燕辽地区燕山期火成岩与造山模型.现代地质,1996,10(02): 137-148
方文昌. 吉林省花岗岩类及成矿作用. 吉林科学技术出版社,1992,1-271
苑凤华,路孝平,乔国华.黑龙江省东南部闹枝沟岩体岩浆混合作用的野外地质学证据.吉林地质,2002,21(1-2)
葛文春,吴福元,周长勇等. 大兴安岭北部塔河花岗岩体的时代及对额尔古纳地块构造归属的制约. 科学通报,2005a, 50(12): 1239-1247
葛文春,吴福元,周长勇等. 大兴安岭中部乌兰浩特地区中生代花岗岩的锆石 U-Pb 年龄及地质意义. 岩石学报,2005b, 21(3): 749-762
黑龙江地矿局. 区域地质调查报告(穆棱镇公社幅和东宁县幅部分).1979.78-103
黑龙江地矿局. 黑龙江省区域地质志.北京:地质出版社,1993,347-418
洪大卫,王式桄,谢锡林等. 兴蒙造山带正 ε(Nd,t )值花岗岩的成因和大陆地壳生长.地学前缘,2000.7(2): 441-456
洪大卫,王式桄,谢锡林等. 从中亚正εNd值花岗岩看超大陆演化和大陆地壳生长的关系.地球学报,2003.77(2):203-209
黄宝春,朱鸿,谭承泽.吉林省东部地区古地磁结果的大地构造意义.地球物理学报,1994.37(增 1):304-315
贾大成. 延吉地体地质特征及构造演化探讨.吉林地质,1995.14(1):40-45
姜开君,周永昶. 吉林珲春地区大荒沟花岗岩岩基的岩浆演化和构造环境.地质论评,1993.39(5):465-475
李之彤,赵春荆. 东北地区的印支运动.地质科学,1985.3:211-223
李之彤,赵春荆. 吉黑东部晚三叠世岩浆岩活动及其与板块构造的关系.中国地质科学院院报,1988.18:21-32
李之彤,朱群. 吉黑东部花岗岩类的稳定同位素组成.岩石矿物学杂志,2001.20 (3):253-259
李锦轶,牛宝贵,宋彪等. 长白山北段地壳的形成与演化.北京:地质出版社,1999.1-137
李双林, 欧阳自远. 兴蒙造山带及邻区的构造格局与构造演化. 海洋地质与第四纪地质, 1998, 18(3): 45-54
李昌年. 火成岩微量元素岩石学.中国地质大学出版社,1992,1pp
李兆鼐等.中国东部中、新生代火成岩及其深部过程.北京:地质出版社,2003,70-75。
刘红涛,翟明国,刘建明等. 华北克拉通北缘中生代花岗岩: 从碰撞后到非造山. 岩石学报2002,18(4):433-448
刘伟,杨进辉,李潮峰. 内蒙赤峰地区若干主干断裂带的构造热年代学. 岩石学报,2003,19(4):717-728
刘先文. 吉林东部若干地质问题讨论.吉林地质科技情报,1994,17-19
刘建峰. 小兴安岭早古生代花岗岩地球化学特征及其构造意义.吉林大学硕士学位论文,2006.
路孝平,吴福元,赵成弼等. 通化地区印支期花岗岩锆石U-Pb年龄及其与大别苏鲁超高压带碰撞造山作用之间的关系.科学通报,2003,48(8):843-849
内蒙古地矿局.内蒙古区域地质志,北京:地质出版社,1991
彭玉鲸,王明胜. 走滑断裂带的两类花岗岩.吉林地质,1998,17(2):22-30
彭玉鲸,刘爱,李文锁等. 吉林省延边地区二叠纪的三类植物群与古陆缘再造.吉林地质,1999,18(1):1-12
裴福萍. 延边地区晚三叠世火山岩的岩石地球化学特征及其构造意义.世界地质,2004,23(1):6-13
齐成栋,纪春华,韩江等.吉林至珲春地区晚二叠世—早三叠世花岗岩成因机制.吉林地质,2005.24 (2):10-15
秦克章,田中亮吏,李伟实,石原舜三.满洲里地区印支期花岗岩Rb-Sr等时线年代学证据,岩石矿物学杂志,199 8 .17(3):235-240
任纪舜,陈延愚,牛宝贵等. 中国东部及邻区大陆岩石圈的构造演化与成矿. 北京: 科学出版社,1990
邵济安,唐克东,詹立培等. 一个古大陆边缘的再造及其大地构造意义——延边地质延吉新进展.中国科学(B 辑).1995.25(5):548-555
石玉若等. 内蒙古苏左旗地区闪长-花岗岩类 SHRIMP 年代学.地质学报,2004.78(6):789-799
史长义,鄢明才,刘崇民等. 中国花岗岩类化学元素丰度及特征.地球化学,2005,34(5):471-782
宋彪, 李锦轶, 牛宝贵等. 黑龙江省东部麻山群黑云斜长片麻岩中锆石的年龄及其地质意义. 地球学报, 1997, 18(3): 306-312
孙革.中国吉林天桥岭晚三叠世植物群.吉林科学技术出版社.1993.1-157
隋振民,葛文春,吴福元等.大兴安岭东北部哈拉巴奇花岗岩体锆石 U- Pb 年龄及其成因.世界地质.2006.25(3):229-236
孙德有,吴福元,李惠民等. 小兴安岭西北部造山后 A 型花岗岩的时代及与索伦山-贺根山-扎赉特碰撞拼合带东延的关系. 科学通报, 2000, 45 (20): 2217-2222
孙德有.张广才岭中生代花岗岩成因及其地球动力学意义. 吉林大学博士学位论文,2001
孙德有,吴福元,张艳斌等. 西拉木伦河-长春-延吉板块缝合带的最后闭合时间—来自吉林大玉山花岗岩体的证据.吉林大学学报(地球科学版),2004,34(2):174-181.
孙德有,吴福元,高山等. 吉林中部晚三叠世和早侏罗世两期铝质 A 型花岗岩的厘定及对吉黑东部构造格局的制约.地学前缘,2005,12(2):263-275
孙德有,吴福元,高山. 小兴安岭东部清水岩体的锆石激光探针 U-Pb 年龄测定.地球学报,2004,25(2):213-218
陶继雄,胡凤翔,陈志勇. 华北陆块北缘印支期S型花岗岩带特征及其构造环境.岩石矿物学杂志,2003,22(2):212-218
陶奎元,毛建仁,杨祝良等. 中国东南部中生代岩石构造组合和复合动力学过程的记录. 地学前缘, 1998, 5(4): 183-190
唐克东,王莹,何国琦等. 中国东北及邻区大陆边缘构造. 地质学报,1995,69(1):16-30
唐克东,邵济安,李景春等. 吉林延边缝合带的性质与东亚构造,地质通报,2004,23(9-10):885-891
吴福元,杨进辉,柳小明. 辽东半岛中生代花岗质岩浆作用的年代学格架. 高校地质学报, 2005,11(3):305-317
吴福元, 江博明, 林强. 中国北方造山带造山后花岗岩的同位素特点与地壳生长意义. 科学通报,1997, 42(20): 2188-2192
吴福元,林强,葛文春等.张广才岭新华屯岩体的形成时代与成因研究. 岩石矿物学杂志, 1998,17(3):226-234
吴福元, SWILDE, 孙德有. 佳木斯地块片麻状花岗岩的锆石离子探针 U-Pb 年龄. 岩石学报, 2001, 17(3): 443-452
吴福元,曹林. 东北亚地区的若干重要基础地质问题. 世界地质, 1999, 18(2): 1-13
吴福元,孙德有,林强. 东北地区显生宙花岗岩成因与地壳增生. 岩石学报,1999,15 (2) : 181-189
王五力,郑少林等.中国东北环太平洋带构造地层学.北京:地质出版社,1995. 160
王友勤. 关于中国东北区地层区划的意见. 吉林地质, 1996.15(3-4): 15-22
王友勤,张德英. 黑龙江省东南部陆相上三叠统德发现.地层学杂志,1984,8(4):308-313
王友勤,殷场健,赵春荆等. 黑龙江省东宁县闹枝沟印支期花岗岩体的发现及其地质意义.中国地质科学院沈阳地矿所所刊,1983.6:57-66
王占福. 延边地区前中生代主要变质岩地质演化特征概述.吉林地质.1998.17(2):31-41
王万军,孙振家,胡祥昭. 内蒙古前进场花岗岩体的地质特征及其构造环境.地质与勘探, 2005,44(2):35-40
王涛. 花岗岩混合成因研究及大陆动力学意义.岩石学报,2000a.16(02):161-168
王涛. 花岗岩研究与大陆动力学.地学前缘,2000b.7(增刊):137-146
武广,孙丰月,赵财胜等. 额尔古纳地块北缘早古生代后碰撞花岗岩的发现及其地质意义. 科学通报,2005,50(20): 2278-2288
杨金中,邱海峻,孙家鹏等. 跃进山岩系及其构造意义. 长春科技大学学报,1998,28:380-385
袁洪林,吴福元,高山等.东北地区新生代侵入体的锆石激光探针 U-Pb 年龄测定与稀土元素成分分析.科学通报,2003,48(14):1511-1520
张兴洲,杨宝俊,吴福元等.中国兴蒙-吉黑地区岩石圈结构基本特征.中国地质.2006.33(4):817-823
张艳斌,吴福元,孙德有等. 延边”早海西期”棉田花岗岩和仲坪紫苏辉石闪长岩的单颗粒锆石 U-Pb 定年.地质论评,2002a,48(4):224-229
张艳斌,吴福元,李惠民等. 吉林黄泥岭花岗岩体的单颗粒锆石 U-Pb 年龄,岩石学报, 2002b ,18 (4) : 475 – 481
张艳斌. 延边地区花岗质岩浆活动的同位素地质年代学格架. 吉林大学博士学位论文,2002c
张艳斌,吴福元,翟明国等. 和龙地块的构造属性与华北地台北缘东段边界.中国科学 D辑,2004,34(9):795-806.
张用焕,彭玉鲸,欧祥喜. 关于吉林省延边地区二叠纪的思考.吉林地质,2000.19(1):1-12
赵成弼,靳克,齐成栋等. 珲春地区早印支期I-A型花岗岩系的特征及其大地构造意义.吉林地质,2001.21(1):1-11
周建波,刘建辉,郑常青等. 大别-苏鲁造山带的东延及板块缝合线:郯庐-鸭绿江-延吉断裂的厘定.高校地质学报,2005.11(1):92-104
Andersen T. Correction of common lead in U-Pb analyses that do not resport 204Pb. Chem.Geol., 2002(192):59-79
Batchelor, B., Bowden, P.. Petrogenetic interpretation of granitoid rock series using multicationic parameters. Chemical Geology, 1985. 48:43–55.
Barbarin, B.. Granitoids: main petrogenetic classifications in relation to origin and tectonic setting. Geol. J, 1990.25, 227–238.
Barbarin,B. A review of the relationships between granitoid types, their origins and their geodynamic environments. Lithos,1999.46:605–626
Barth A.P., Wooden J.L., Tosda R.M. and Morrison,J. Crustal contamination in the petrogenesis of a calc-alkalic rock series:Josephine Mountain intrusion, Califo rnia. GSA Bulletin, 1995. 107(2) : 201- 212
Bartholomew, D.S., Tarney, J. Geochemical characteristics of magmatism in the southern Andes 45–46°S . Andean magmatism:chemical and isotopic constraints,1984.In: Harmon, R.S., Barreiro, B.A. Eds. , Shiva Publ., Nantwich, pp. 220-229.
Bateman, P.C., A summary of critical relations in the central part of the Sierra Nevada Batholith California, USA.Geol. Soc. Am. Mem,1983.159:241–254.
Bateman, P.C. Plutonism in the central part of the Sierra Nevada Batholith, California. US Geol. Surv. Prof,1992.Paper 1483:1–186
Boriani A.Origoni E.G and Pinarell L. Paleozoic evolution of southern Alpine crust (northern Italy ) as indicated by constrasting granitoid suites. Lithos,1995.35: 47～ 63
Castro A. H-type (Hybrid) granitoids: aproposed revision of the granite type classification and nomenclature. Earth Science Reviews, 1991. 31: 237～ 253
CollinsW J. S-and I-type granites of the eastern Lachlan fold belt: products of tree- component mixing. Transaction of the Royal Society of Edinburgh, Earth Sciences, 1996. 88: 171-179
Collins W J. Evaluation of petrogenetic models for Lachlan Fold Belt granitoids: implications for crustal architecture and tectonic models. Australian Journal of Sciences, 1998. 45: 483～ 500
Desouky M.D., Feely M. and Mortr P. Diorite-granite magma mingling and mixing along the axis of Galway Granite batholith,Ireland. Journal of the Society London, 1996. 153: 361-374
Faure M,Lin W,Le Breton N.Where is the North China-South China block boundary in eastern China? Geology,2001. 29: 119-122
Jahn, B.M., Wu, F.Y., Hong, D.W., Important crustal growth in the Phanerozoic: isotopic evidence of granitoids from East- central Asia.Proc. Indian Acad. Sci., Earth Planet. Sci., 2000a.109, 5-20.
Jahn, B.M., Wu, F.Y., Chen, B.,. Granitoids of the Central Asian Orogenic Belt and continental growth in the Phanerozoic. Trans. R. Soc. Edinb.: Earth Sci. ,2000c. 91, 181- 193.
Keay S, CollinsW J and Mc Culloch M T. A three-component mixing model for granitoid genesis: Lachlan Fold Belt, eastern Australia. Geology, 1997. 25: 307～310
Kovalenko, V.I., Yarmolyuk, V.V., Kovach, V.P., Kotov, A.B., Kozakov,I.K., Sal’nikova, E.B., 1996. Sources of Phanerozoic granitoids in Central Asia: Sm–Nd isotope data. Geochem.Int. 34, 628– 640.
M. Arslan, Z. Aslan.Mineralogy, petrography and whole-rock geochemistry of the Tertiary granitic intrusions in the Eastern Pontides, Turkey, Journal of Asian Earth Sciences ,2006.27 :177–193
Maruyama S. Pacific-type orogeny revisited: Miyashiro-type orogeny proposed. The Island Arc, 1997, 6: 91-120
Pearce, J.A., Harris, N.B.W., Tindle, A.G.. Trace element discrimination diagrams for the tectonic interpretation ofgranitic rocks. J. Petrol , 1984 .25, 956–983.
Pitcher, W.S... Granite Type and Tectonic Environment. In: Hsu, K. Ed. , Mountain Building Processes, Academic Press,London ,1983 .pp. 19–40.
Pitcher, W.S., Granites and yet more granites forty years on.Geol. Rundschau 1987. 76, 51–79.
Pitcher, W.S., The Nature and Origin of Granite. Blackie Acad. and Prof. ed., London, 1993.
Pitcher,W.S. The Nature and Origin of Granite. London:Chapman and Hall. 1997.
Soesoo A , Bons P D and Gray D R. Divergent double subduction: Tectonic and petrology consequences. Geology, 1997. 25: 755～758
Simon A. Wilde.Late Pan-African magmatism in northeastern China: SHRIMP U–Pb zircon evidence from granitoids in the Jiamusi Massif.Precambrian Research.2003.122 (2003) 311–327
Wilde, S.A., Wu, F.Y., Zhang, X.Z., The Mashan Complex:SHRIMP U–Pb zircon evidence for a Late Pan-Africanmetamorphic event in NE China and its implications for global continental reconstructions. Geochimica ,2001.30, 35–50 (in Chinese, with English abstract).}
Wiedenbeck M, Alle P, Corfu F et al. Three natural zircon standards for U-Th-Pb, Lu-Hf, trace element and REE analyses. Geostand Newsl, 1995(19): 1-23
Wu, F.-Y. et al..A-type granites in northeastern China:age and geochemical constraints on their petrogenesis, Chemical Geology ,2002.187,143-173
Wu, F.-Y. et al. Highly fractionated I-type granites in NE China(Ⅰ ): geochronology and petrogenesis. Lithos, 2003.66:241- 273
Wu, F.-Y. et al. Highly fractionated I-type granites in NE China(Ⅱ ):isotopic geochemistry and implications for crustal growth in the Phanerozoic.Lithos,2003 .67:191– 204
Wu, F.-Y. et al., The Hulan Group: Its role in the evolution of the Central Asian Orogenic Belt of NE China, Journal of Asian Earth Sciences (2007), doi:10.1016/j. jseaes.2007.01.003
Wu, F.-Y. et al. Initial constraints on the timing of granitic magmatism in North Korea using U–Pb zircon geochronology. Chem. Geol. 2007,doi:10.1016/j.chemgeo .2006.11.012
Yoji Arakawa.Two types of granitic intrusions in the Hida belt,Japan:Sr isotopic and chemical characteristics of the Mesozoic Funatsu granitic rocks.Chemical Geology, 1990.85:101-117.
Yoji Arakawa, Taro Shinmura.Nd-Sr isotopic and geochemical characteristics of two contrasting types of calc-alkaline plutons in the Hida belt,Japan,Chemical Geology, 1995.124: 217-232
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