|Table of Contents|

Zircon U-Pb Dating and Geochemical Characteristics of Zaohuogou Granitoids in the Middle Part of East Kunlun, China and Their Tectonic Significance(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2020年第05期
Page:
603-621
Research Field:
基础地质与矿产地质
Publishing date:

Info

Title:
Zircon U-Pb Dating and Geochemical Characteristics of Zaohuogou Granitoids in the Middle Part of East Kunlun, China and Their Tectonic Significance
Author(s):
JIAN Kun-kun12 HE Yuan-fang12 ZHAO Duan-chang12 GAO Feng12 WANG Xing12 YUAN Zhang12
1. Shaanxi Institute of Geological Survey, Xi’an 710054, Shaanxi, China; 2. Shaanxi Mineral Resources and Geological Survey, Xi’an 710068, Shaanxi, China
Keywords:
I-type granitoid geochemistry zircon U-Pb age petrogenesis Middle Permian magma mixing continental arc East Kunlun
PACS:
P595; P597
DOI:
10.19814/j.jese.2020.08022
Abstract:
Zaohuogou granitoids in the middle part of East Kunlun consist of quartz-diorite, tonalite, granodiorite and monzogranite. The rocks are characterized by variable SiO2 contents(60.94%-74.14%), moderate to high Al2O3 and total alkaline(the contents of Al2O3 and Na2O+K2O are 12.73%-16.22% and 4.51%-7.61%), suggesting that Zaohuogou granitoids belong to I-type with middle-high potassium calc-alkaline and meta-aluminous to weak peraluminous. The total content of REE is low((106.62-182.76)×10-6)with an average of 144.25×10-6. They are characterized by relative enrichment in large ion lithophile elements(LILEs)and light rare earth elements(LREEs), but depletion in high field strength elements(HFSEs), in addition, they show Ti, Nb and Ta negative anomaly on the primitive mantle-normalized trace element spider diagram. LA-ICP-MS Zircon U-Pb dating shows that Zaohuogou granitoids are formed in 262-260 Ma, belong to the late Middle Permian. The geochemical characteristics indicate that the granitoids are formed in a continental margin arc environment. Combined with the regional geological background and previous data, it is suggested that the Paleotethys ocean begins to subduct northward beneath East Kunlun terrane in the late Middle Permian. During the subduction of Paleotethys ocean, the mantle-derived melts intrude into the lower crust and result in partial melting of lower crust leading to development of granitic magma. The magma is formed by magma mixing of the mantle-derived and crust-derived melts, then experiences some degree of crystallization differentiation, and finally consolidates into the granitoids.

References:

[1] 殷鸿福,张克信.东昆仑造山带的一些特点[J].地球科学,1997,22(4):339-342.
YIN Hong-fu,ZHANG Ke-xin.Characteristics of the Eastern Kunlun Orogenic Belt[J].Earth Science,1997,22(4):339-342.
[2] YANG J S,ROBINSON P T,JIANG C F,et al.Ophiolites of the Kunlun Mountains,China and Their Tectonic Implications[J].Tectonophysics,1996,258(1/2/3/4):215-231.
[3] 国显正,贾群子,李金超,等.东昆仑扎玛休玛正长花岗岩年代学、地球化学特征及其构造意义[J].地质学报,2019,93(4):830-842.
GUO Xian-zheng,JIA Qun-zi,LI Jin-chao,et al.Geochronology and Geochemical Characteristics of Syenogranite from the Zhamaxiuma Area in East Kunlun and Their Tectonic Significance[J].Acta Geologica Sinica,2019,93(4):830-842.
[4] 韩建军,李运冬,宋传中,等.东昆仑东段都兰热水花岗岩锆石U-Pb年龄、地球化学及构造意义[J].地质学报,2020,94(3):768-781.
HAN Jian-jun,LI Yun-dong,SONG Chuan-zhong,et al.Zircon U-Pb Dating and Geochemistry of Gra-nite in the Reshui Area of Dulan County,Eastern Section of East Kunlun Orogen and Its Tectonic Implications[J].Acta Geologica Sinica,2020,94(3):768-781.
[5] 张新远,李五福,欧阳光文,等.东昆仑东段青海战红山地区早三叠世火山岩的发现及其地质意义[J].地质通报,2020,39(5):631-641.
ZHANG Xin-yuan,LI Wu-fu,OUYANG Guang-wen,et al.The Discovery of Early Triassic Volcanic Rocks in Zhanhongshan Area of Qinghai Province in the Eastern Section of East Kunlun Mountain and Its Geolo-gical Significance[J].Geological Bulletin of China,2020,39(5):631-641.
[6] 许志琴,杨经绥,李海兵,等.造山的高原:青藏高原的地体拼合、碰撞造山及隆升机制[M].北京:地质出版社,2006.
XU Zhi-qin,YANG Jing-sui,LI Hai-bing,et al.Orogenic Plateaux:The Mechanism of Terrane Amalgamation,Collisional and Uplift in Qinghai-Tibet Plateau[M].Beijing:Geological Publishing House,2006.
[7] 孙 雨,裴先治,丁仨平,等.东昆仑哈拉尕吐岩浆混合花岗岩:来自锆石U-Pb年代学的证据[J].地质学报,2009,83(7):1000-1010.
SUN Yu,PEI Xian-zhi,DING Sa-ping,et al.Halagatu Magma Mixing Granite in the East Kunlun Mountains:Evidence from Ziron U-Pb Dating[J].Acta Geologica Sinica,2009,83(7):1000-1010.
[8] 熊富浩,马昌前,张金阳,等.东昆仑造山带早中生代镁铁质岩墙群LA-ICP-MS锆石U-Pb定年、元素和Sr-Nd-Hf同位素地球化学[J].岩石学报,2011,27(11):3350-3364.
XIONG Fu-hao,MA Chang-qian,ZHANG Jin-yang,et al.LA-ICP-MS Zircon U-Pb Dating,Elements and Sr-Nd-Hf Isotope Geochemistry of the Early Mesozoic Mafic Dyke Swarms in East Kunlun Orogenic Belt[J].Acta Petrologica Sinica,2011,27(11):3350-3364.
[9] 陈国超.东昆仑造山带(东段)晚古生代—早中生代花岗质岩石特征、成因及地质意义[D].西安:长安大学,2014.
CHEN Guo-chao.Petrology,Genesis and Geological Significance of Late Paleozoic-Early Mesozoic Grani-toids in East Kunlun Orogen[D].Xi’an:Chang’an University,2014.
[10] 菅坤坤,朱云海,王利伟,等.东昆仑中灶火地区中三叠世花岗岩LA-ICP-MS锆石U-Pb定年、岩石成因及构造意义[J].地质论评,2017,63(3):659-676.
JIAN Kun-kun,ZHU Yun-hai,WANG Li-wei,et al.Zircon LA-ICP-MS Age Dating,Petrogenesis and Tectonic Implications of the Middle Triassic Granites from the Zhongzaohuo Area,East Kunlun[J].Geological Review,2017,63(3):659-676.
[11] 罗明非,莫宣学,喻学惠,等.东昆仑香日德地区晚三叠世花岗岩LA-ICP-MS锆石U-Pb定年、岩石成因和构造意义[J].岩石学报,2014,30(11):3229-3241.
LUO Ming-fei,MO Xuan-xue,YU Xue-hui,et al.Zircon LA-ICP-MS U-Pb Age Dating,Petrogenesis and Tectonic Implications of the Late Triassic Granites from the Xiangride Area,East Kunlun[J].Acta Petrologica Sinica,2014,30(11):3229-3241.
[12] 孔会磊,李金超,栗亚芝,等.青海东昆仑东段加当辉长岩LA-ICP-MS锆石U-Pb测年及其地质意义[J].地质与勘探,2017,53(5):889-902.
KONG Hui-lei,LI Jin-chao,LI Ya-zhi,et al.Zircon LA-ICP-MS U-Pb Dating and Its Geological Significance of the Jiadang Gabbro in the Eastern Section of the East Kunlun,Qinghai Province[J].Geology and Exploration,2017,53(5):889-902.
[13] 邓文兵,裴先治,刘成军,等.东昆仑东段香日德地区察汗陶勒盖正长花岗岩LA-ICP-MS锆石U-Pb年龄及其地质意义[J].地质通报,2016,35(5):687-699.
DENG Wen-bing,PEI Xian-zhi,LIU Cheng-jun,et al.LA-ICP-MS Zircon U-Pb Dating of the Chahantaolegai Syenogranites in Xiangride Area of East Kunlun and Its Geological Significance[J].Geological Bulletin of China,2016,35(5):687-699.
[14] 李玉龙,蔡生顺,常 涛,等.东昆仑东段中二叠世洋陆俯冲的新证据:来自希望沟辉长岩U-Pb年龄的约束[J].矿物岩石,2018,38(1):91-98.
LI Yu-long,CAI Sheng-shun,CHANG Tao,et al.The New Evidence of Permian Ocean-continent Subduction in the East Section of East Kunlun:Constraint from U-Pb Age Dating of Xiwanggou Gabbro[J].Journal of Mineralogy and Petrology,2018,38(1):91-98.
[15] 张志清,陈 静,余福承,等.东昆仑希望沟中二叠世辉长岩Sr-Nd-Lu-Hf同位素特征及其地质意义[J].矿物岩石,2019,39(3):26-31.
ZHANG Zhi-qing,CHEN Jing,YU Fu-cheng,et al.Sr-Nd-Lu-Hf Isotopic Characteristics and Geological Significance of the Middle Permian Gabbro in Xiwanggou Area,East Kunlun[J].Journal of Mineralogy and Petrology,2019,39(3):26-31.
[16] HUANG H,NIU Y L,NOWELL G,et al.Geochemical Constraints on the Petrogenesis of Granitoids in the East Kunlun Orogenic Belt,Northern Tibetan Plateau:Implications for Continental Crust Growth Through Syn-collisional Felsic Magatism[J].Chemical Geology,2014,370:1-18.
[17] DING Q F,JIANG S Y,SUN F Y.Zircon U-Pb Geochronology,Geochemical and Sr-Nd-Hf Isotopic Compositions of the Triassic Granite and Diorite Dikes from the Wulonggou Mining Area in the Eastern Kunlun Orogen,NW China:Petrogenesis and Tecto-nic Implications[J].Lithos,2014,205:266-283.
[18] 陈国超,裴先治,李瑞保,等.东昆仑东段可日正长花岗岩年龄和岩石成因对东昆仑中三叠世构造演化的制约[J].岩石学报,2018,34(3):567-585.
CHEN Guo-chao,PEI Xian-zhi,LI Rui-bao,et al.Age and Lithogenesis of Keri Syenogranite from Eastern Part of East Kunlun Orogenic Belt:Constraint on the Middle Triassic Tectonic Evolution of East Kunlun[J].Acta Petrologica Sinica,2018,34(3):567-585.
[19] 陈国超,裴先治,李瑞保,等.东昆仑古特提斯后碰撞阶段伸展作用:来自晚三叠世岩浆岩的证据[J].地学前缘,2019,26(4):191-208.
CHEN Guo-chao,PEI Xian-zhi,LI Rui-bao,et al.Lithospheric Extension of the Post-collision Stage of the Paleo-Tethys Oceanic System in the East Kunlun Orogenic Belt:Insights from Late Triassic Plutons[J].Earth Science Frontiers,2019,26(4):191-208.
[20] 王 珂,王连训,马昌前,等.东昆仑加鲁河中三叠世含石榴石二云母花岗岩的成因及地质意义[J].地球科学,2020,45(2):400-418.
WANG Ke,WANG Lian-xun,MA Chang-qian,et al.Petrogenesis and Geological Implications of the Middle Triassic Garnet-bearing Two-mica Granite from Jialuhe Region,East Kunlun[J].Earth Science,2020,45(2):400-418.
[21] 俞军真,郑有业,许荣科,等.东昆仑东段将军墓含矿岩体锆石U-Pb年代学、地球化学特征及其地质意义[J].地球科学,2020,45(4):1151-1167.
YU Jun-zhen,ZHENG You-ye,XU Rong-ke,et al.Zircon U-Pb Chronology,Geochemistry of Jiangjunmu Ore-bearing Pluton,Eastern Part of East Kunlun and Their Geological Significance[J].Earth Science,2020,45(4):1151-1167.
[22] 李积清,王 涛,陈 静,等.东昆仑马尼特金矿床赋矿花岗闪长岩锆石U-Pb年龄及岩石地球化学特征[J].矿物岩石,2019,39(3):69-77.
LI Ji-qing,WANG Tao,CHEN Jing,et al.Zircon U-Pb Age and Petrogeochemical Characteristics of Ore-hosting Granodiorite in Manite Gold Deposit,East Kunlun[J].Journal of Mineralogy and Petrology,2019,39(3):69-77.
[23] 顾 焱,钱 烨,李予晋,等.东昆仑骆驼峰地区中晚三叠世花岗岩年代学、地球化学及构造意义[J].矿产勘查,2019,10(4):724-736.
GU Yan,QIAN Ye,LI Yu-jin,et al.Geochronology,Geochemistry and Tectonic Significance of Middle and Late Triassic Granites in the Luotuofeng Area,East Kunlun[J].Mineral Exploration,2019,10(4):724-736.
[24] 许志琴,李海兵,杨经绥.造山的高原:青藏高原巨型造山拼贴体和造山类型[J].地学前缘,2006,13(4):1-17.
XU Zhi-qin,LI Hai-bing,YANG Jing-sui.An Oroge-nic Plateau:The Orogenic Collage and Orogenic Types of the Qinghai-Tibet Plateau[J].Earth Science Frontiers,2006,13(4):1-17.
[25] 王旭斌,裴先治,李瑞保,等.青海东昆仑东段塔妥地区小庙岩组变质岩LA-ICP-MS锆石U-Pb年龄及其地质意义[J].地质通报,2016,35(7):1144-1157.
WANG Xu-bin,PEI Xian-zhi,LI Rui-bao,et al.LA-ICP-MS Zircon U-Pb Ages of Metamorphic Rocks from Xiaomiao Formation in Tatuo Area of Eastern East Kunlun Mountains and Their Geological Significance[J].Geological Bulletion of China,2016,35(7):1144-1157.
[26] LIU Y S,HU Z C,GAO S,et al.In-situ Analysis of Major and Trace Elements of Anhydrous Minerals by LA-ICP-MS Without Applying an Internal Standard[J].Chemical Geology,2008,257(1/2):34-43.
[27] HOSKIN P W O,SCHALTEGGER U.The Composition of Zircon and Igneous and Metamorphic Petrogenesis[J].Reviews in Mineralogy and Geochemistry,2003,53(1):27-62.
[28] 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):1589-1604.
WU Yuan-bao,ZHENG Yong-fei.Mineral Study of Genesis of Zircon and Its Constraints on Interpretation of U-Pb Age[J].Chinese Science Bulletin,2004,49(16):1589-1604.
[29] 施 彬,刘 力.东昆仑灶火沟早志留世花岗岩岩石学、地球化学特征及地质意义[J].世界地质,2014,33(4):758-767.
SHI Bin,LIU Li.Petrological and Geochemical Cha-racteristics of Early Silurian Granites in Zaohuogou of Eastern Kunlun and Their Geological Significance[J].World Geology,2014,33(4):758-767.
[30] BELOUSOVA E,GRIFFIN W,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(5):602-622.
[31] 钟玉芳,马昌前,佘振兵.锆石地球化学特征及地质应用研究综述[J].地质科技情报,2006,25(1):27-34,40.
ZHONG Yu-fang,MA Chang-qian,SHE Zhen-bing.Geochemical Characteristics of Zircon and Its Applications in Geosciences[J].Geological Science and Technology Information,2006,25(1):27-34,40.
[32] MIDDLEMOST E A K.Naming Materials in the Magma/Igneous Rock System[J].Earth-science Reviews,1994,37(3/4):215-224.
[33] PECCERILLO A,TAYLOR S R.Geochemistry of Eocene Calc-alkaline Volcanic Rocks from Kastamonu Area,Northern Turkey[J].Contributions to Minera-logy and Petrology,1976,58:63-81.
[34] MANIAR P D,PICCOLI P M.Tectonic Discrimination of Granitoids[J].Bulletin of the Geological Society of America,1989,101(5):635-643.
[35] SUN S S,MCDONOUGH W F.Chemical and Isoto-pic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes[J].Geological Society,London,Special Publications,1989,42:313-345.
[36] BONIN B.A-type Granites and Related Rocks:Evolution of a Concept,Problems and Prospects[J].Lithos,2007,97(1/2):1-29.
[37] 吴福元,李献华,郑永飞,等.Lu-Hf同位素体系及其岩石学应用[J].岩石学报,2007,23(2):185-220.
WU Fu-yuan,LI Xian-hua,ZHENG Yong-fei,et al.Lu-Hf Isotopic Systematics and Their Applications in Petrology[J].Acta Petrologica Sinica,2007,23(2):185-220.
[38] WHALEN J B,CURRIE K L,CHAPPELL B W.A-type Granites:Geochemical Characteristics,Discrimination and Petrogenesis[J].Contributions to Minera-logy and Petrology,1987,95:407-419.
[39] SYLVESTER P J.Post-collisional Strongly Peraluminous Gra-nites[J].Lithos,1998,45(1/2/3/4):29-44.
[40] CHAPPELL B W,WHITE A J R.I- and S-type Gra-nites in the Lachlan Fold Belt[J].Transactions of the Royal Society of Edinburgh:Earth Sciences,1992,83:1-26.
[41] 邓晋福,刘 翠,冯艳芳,等.关于火成岩常用图解的正确使用:讨论与建议[J].地质论评,2015,61(4):717-734.
DENG Jin-fu,LIU Cui,FENG Yan-fang,et al.On the Correct Application in the Common Igneous Petrolo-gical Diagrams:Discussion and Suggestion[J].Geological Review,2015,61(4):717-734.
[42] CHAPPELL B W.Aluminum Saturation in I- and S-type Granite and the Characterization of Fractionated Haplongranite[J].Lithos,1999,46(3):535-551.
[43] MA C Q,LI Z C,EHLERS C,et al.A Post-collisional Magmatic Plumbing System:Mesozoic Granitoid Plutons from the Dabieshan High-pressure and Ultrahigh-pressure Metamorphic Zone,East-central China[J].Lithos,1998,45(1/2/3/4):431-456.
[44] ALTHERR R,SIEBEL W.I-type Plutonism in a Continental Back-arc Setting:Miocene Granitoids and Monzonites from the Central Aegean Sea,Greece[J].Contributions to Mineralogy and Petrology,2002,143(4):397-415.
[45] KAYGUSUZ A,SIEBEL W,SEN C,et al.Petrochemistry and Petrology of I-type Granitoids in an Arc Setting:The Composite Torul Pluton,Eastern Pontides,NE Turkey[J].International Journal of Earth Sciences,2008,97(4):739-764.
[46] RUDNICK R L.Making Continental Crust[J].Nature,1995,378:571-577.
[47] TAYLOR S R,MCCLENNAN S M.The Continental Crust:Its Composition and Evolution[M].Blackwell:Oxford Press,1985.
[48] GREEN T H.Significance of Nb/Ta as an Indicator of Geochemical Processes in the Crust-mantle System[J].Chemical Geology,1995,120(3/4):347-359.
[49] HOFMANN A W.Chemical Differentiation of the Earth:The Relationship Between Mantle,Continental Crust,and Oceanic Crust[J].Earth and Planetary Science Letters,1988,90(3):297-314.
[50] 莫宣学,罗照华,邓晋福,等.东昆仑造山带花岗岩及地壳生长[J].高校地质学报,2007,13(3):403-414.
MO Xuan-xue,LUO Zhao-hua,DENG Jin-fu,et al.Granitoids and Crustal Growth in the East-Kunlun Orogenic Belt[J].Geological Journal of China Universities,2007,13(3):403-414.
[51] 刘成东,莫宣学,罗照华,等.东昆仑造山带花岗岩类Pb-Sr-Nd-O同位素特征[J].地球学报,2003,24(6):584-588.
LIU Cheng-dong,MO Xuan-xue,LUO Zhao-hua,et al.Pb-Sr-Nd-O Isotope Characteristics of Granitoids in East Kunlun Orogenic Belt[J].Acta Geoscientica Sinica,2003,24(6):584-588.
[52] 刘成东,莫宣学,罗照华,等.东昆仑壳-幔岩浆混合作用:来自锆石SHRIMP年代学的证据[J].科学通报,2004,49(6):596-602.
LIU Cheng-dong,MO Xuan-xue,LUO Zhao-hua,et al.Mixing Events Between the Crust- and Mantle-derived Magmas in East Kunlun Mountains:Evidence from Zircon SHRIMP Geochronology[J].Chinese Science Bulletin,2004,49(6):596-602.
[53] 谌宏伟,罗照华,莫宣学,等.东昆仑造山带三叠纪岩浆混合成因花岗岩的岩浆底侵作用机制[J].中国地质,2005,32(3):386-395.
CHEN Hong-wei,LUO Zhao-hua,MO Xuan-xue,et al.Underplating Mechanism of Triassic Granite of Magma Mixing Origin in the East Kunlun Orogenic Belt[J].Geology in China,2005,32(3):386-395.
[54] 张爱奎,刘光莲,莫宣学,等.青海祁漫塔格晚古生代—早中生代侵入岩构造背景与成矿关系[J].西北地质,2012,45(1):9-19.
ZHANG Ai-kui,LIU Guang-lian,MO Xuan-xue,et al.Relationship Between Tectonic Settings and Metallo Genesis of Late Paleozoic-Early Mesozoic Intrusive Rock in Qimantage,Qinghai Province[J].Northwestern Geology,2012,45(1):9-19.
[55] ZHANG J Y,MA C Q,XIONG F H,et al.Petrogenesis and Tectonic Significance of the Late Permian-Middle Triassic Calc-alkaline Granites in the Balong Region,Eastern Kunlun Orogen,China[J].Geological Magazine,2012,149(5):892-908.
[56] 马昌前,熊富浩,张金阳,等.从板块俯冲到造山后阶段俯冲板片对岩浆作用的影响:东昆仑早二叠世—晚三叠世镁铁质岩墙群的证据[J].地质学报,2013,87(增):78-81.
MA Chang-qian,XIONG Fu-hao,ZHANG Jin-yang,et al.The Influence of Subduction Plate on Magmatism from Plate Subduction to Post Orogenic Stage:Evidence from Early Permian-Late Triassic Mafic Dyke Swarms in East Kunlun[J].Acta Geolo-gica Sinica,2013,87(S):78-81.
[57] 马圣钞,丰成友,李大新,等.青海祁漫塔格虎头崖矿区花岗岩地球化学特征及构造意义[J].地质学报,2014,88(1):72-82.
MA Sheng-chao,FENG Cheng-you,LI Da-xin,et al.Geochemical Characteristics of Granite in Hutouya Mining Area of Qimantag,Qinghai and Its Constraints on Tectonic Setting[J].Acta Geologica Sinica,2014,88(1):72-82.
[58] 罗照华,柯 珊,曹永清,等.东昆仑印支晚期幔源岩浆活动[J].地质通报,2002,21(6):292-297.
LUO Zhao-hua,KE Shan,CAO Yong-qing,et al.Late Indosinian Mantle-derived Magmatism in the East Kunlun[J].Geological Bulletin of China,2002,21(6):292-297.
[59] WU F Y,JAHN B M,WILDE S A,et al.Highly Fractionated I-type Granites in NE China(I):Geochrono-logy and Petrogenesis[J].Lithos,2003,66(3/4):241-273.
[60] 王永标.巴颜喀拉及邻区中二叠世古海山的结构与演化[J].中国科学:D辑,地球科学,2005,35(12):1140-1149.
WANG Yong-biao.Structure and Evolution of Middle Permian Paleo-seamounts in Bayan Har and Its Adjacent Areas[J].Science in China:Series D,Earth Sciences,2005,35(12):1140-1149.
[61] 郭安林,张国伟,孙延贵,等.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[J].中国科学:D辑,地球科学,2006,36(7):618-629.
GUO An-lin,ZHANG Guo-wei,SUN Yan-gui,et al.Geochemistry and Spatial Distribution of OIB and MORB in A’nyemaqen Ophiolite Zone:Evidence of Majixueshan Ancient Ridge-centered Hotspot[J].Science in China:Series D,Earth Sciences,2006,36(7):618-629.
[62] 刘战庆,裴先治,李瑞保,等.东昆仑南缘布青山构造混杂岩带的地质特征及大地构造意义[J].地质通报,2011,30(8):1182-1195.
LIU Zhan-qing,PEI Xian-zhi,LI Rui-bao,et al.Geological Characteristics of the Buqingshan Tectonic Mélange Belt in the Southern Margin of East Kunlun and Its Tectonic Implications[J].Geological Bulletin of China,2011,30(8):1182-1195.
[63] 刘战庆,裴先治,李瑞保,等.东昆仑南缘阿尼玛卿构造带布青山地区两期蛇绿岩的LA-ICP-MS锆石U-Pb定年及其构造意义[J].地质学报,2011,85(2):185-194.
LIU Zhan-qing,PEI Xian-zhi,LI Rui-bao,et al.LA-ICP-MS Zircon U-Pb Geochronology of the Two Suites of Ophiolites at the Buqingshan Area of the A’nyemaqen Orogenic Belt in the Southern Margin of East Kunlun and Its Tectonic Implication[J].Acta Geologica Sinica,2011,85(2):185-194.
[64] 李瑞保,裴先治,李佐臣,等.东昆仑南缘布青山构造混杂岩带哥日卓托洋岛玄武岩地球化学特征及构造意义[J].地学前缘,2014,21(1):183-195.
LI Rui-bao,PEI Xian-zhi,LI Zuo-chen,et al.Geochemical Characteristics of Gerizhuotuo OIB and Its Tectonic Significance in Buqingshan Tectonic Mélange Belt,Southern Margin of East Kunlun Orogen[J].Earth Science Frontiers,2014,21(1):183-195.
[65] 裴先治.勉略—阿尼玛卿构造带的形成演化与动力学特征[D].西安:西北大学,2001.
PEI Xian-zhi.Geological Evolution and Dynamics of the Mianlue-A’nyemaqen Tectonic Zone,Central China[D].Xi’an:Northwest University,2001.
[66] 郭正府,邓晋福,许志琴,等.青藏东昆仑晚古生代末—中生代中酸性火成岩与陆内造山过程[J].现代地质,1998,12(3):344-352.
GUO Zheng-fu,DENG Jin-fu,XU Zhi-qin,et al.Late Palaeozoic-Mesozoic Intracontinental Orogenic Process and Intermediate-acidic Igneous Rocks from the Eastern Kunlun Mountains of Northwestern China[J].Geoscience,1998,12(3):344-352.
[67] 杨经绥,许志琴,李海兵,等.东昆仑阿尼玛卿地区古特提斯火山作用和板块构造体系[J].岩石矿物学杂志,2005,24(5):369-380.
YANG Jing-sui,XU Zhi-qin,LI Hai-bing,et al.The Paleo-Tethyan Volcanism and Plate Tectonic Regime in the A’nyemaqen Region of East Kunlun,Northern Tibet Plateau[J].Acta Petrologica et Mineralogica,2005,24(5):369-380.
[68] 菅坤坤,魏燕霞,施 彬,等.东昆仑造山带中灶火地区早中生代镁铁质岩墙群的成因及地质意义[J].中国地质,2015,42(5):1457-1470.
JIAN Kun-kun,WEI Yan-xia,SHI Bin,et al.Petrogenesis and Geological Significance of the Early Mesozoic Mafic Dyke Swarms in Zhongzaohuo Area,East Kunlun Orogenic Belt[J].Geology in China,2015,42(5):1457-1470.
[69] 李瑞保.东昆仑造山带(东段)晚古生代—早中生代造山作用研究[D].西安:长安大学,2012.
LI Rui-bao.Research on the Late Paleozoic-Early Mesozoic Orogeny in East Kunlun Orogen[D].Xi’an:Chang’an University,2012.
[70] 赵 旭,付乐兵,魏俊浩,等.东昆仑按纳格角闪辉长岩体地球化学特征及其对古特提斯洋演化的制约[J].地球科学,2018,43(2):354-370.
ZHAO Xu,FU Le-bing,WEI Jun-hao,et al.Geochemical Characteristics of Annage Hornblende Gabbro from East Kunlun Orogenic Belt and Its Constraints on Evolution of Paleo-Tethys Ocean[J].Earth Science,2018,43(2):354-370.
[71] 封 铿,李瑞保,裴先治,等.东昆仑造山带东段大格勒花岗岩锆石U-Pb年代学、地球化学特征及其构造意义[J].地球科学与环境学报,2020,42(4):442-463.
FENG Keng,LI Rui-bao,PEI Xian-zhi,et al.Zircon U-Pb Dating and Geochemical Characteristics of Dagele Granite in the Eastern Margin of East Kunlun Orogenic Belt,China and Their Tectonic Implications[J].Journal of Earth Sciences and Environment,2020,42(4):442-463.
[72] 史连昌,常革红,祁生胜,等.东昆仑大灶火沟—万宝沟晚二叠世陆缘弧火山岩的发现及意义[J].地质通报,2016,35(7):1115-1122.
SHI Lian-chang,CHANG Ge-hong,QI Sheng-sheng,et al.The Discovery of Dazaohuogou-Wanbaogou Late Permian Epicontinental Arc Volcanic Rocks in Eastern Kunlun Mountains and Its Significance[J].Geological Bulletin of China,2016,35(7):1115-1122.
[73] 王 兴,裴先治,李瑞保,等.东昆仑东段下三叠统洪水川组砾岩源区研究:来自砾岩特征及锆石U-Pb年龄的证据[J].中国地质,2019,46(1):155-177.
WANG Xing,PEI Xian-zhi,LI Rui-bao,et al.Conglomerate Source and Source Area Property of Lower Hongshuichuan Formation in the East Kunlun Mountains:Evidence from Conglomerate Characteristics and U-Pb Dating[J].Geology in China,2019,46(1):155-177.
[74] 李瑞保,裴先治,李佐臣,等.东昆仑东段下三叠统洪水川组沉积序列与盆地构造原型恢复[J].地质通报,2015,34(12):2302-2314.
LI Rui-bao,PEI Xian-zhi,LI Zuo-chen,et al.The Depositional Sequence and Prototype Basin for Lower Triassic Hongshuichuan Formation in the Eastern Segment of East Kunlun Mountains[J].Geological Bulletin of China,2015,34(12):2302-2314.
[75] 闫 臻,边千韬,KORCHAGIN O A,等.东昆仑南缘早三叠世洪水川组的源区特征:来自碎屑组成、重矿物和岩石地球化学的证据[J].岩石学报,2008,24(5):1068-1078.
YAN Zhen,BIAN Qian-tao,KORCHAGIN O A,et al.Provenance of Early Triassic Hongshuichuan Formation in the Southern Margin of the East Kunlun Mountains:Constrains from Detrital Framework,Heavy Mineral Analysis and Geochemistry[J].Acta Petrologica Sinica,2008,24(5):1068-1078.
[76] 杨忠智.东昆仑造山带东段下三叠统洪水川组地质特征及构造环境研究[D].西安:长安大学,2012.
YANG Zhong-zhi.A Study on Geologic Feature and Structural Setting of the Lower Triassic Hongshuichuan Formation in Eastern Section of the East Kunlun Orogen[D].Xi’an:Chang’an University,2012.
[77] 罗照华,邓晋福,曹永清,等.青海省东昆仑地区晚古生代—早中生代火山活动与区域构造演化[J].现代地质,1999,13(1):51-56.
LUO Zhao-hua,DENG Jin-fu,CAO Yong-qing,et al.On Late Paleozoic-Early Mesozoic Volcanism and Regional Tectonic Evolution of Eastern Kunlun,Qinghai Province[J].Geoscience,1999,13(1):51-56.
[78] 肖庆辉,邓晋福,邱瑞照,等.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[J].中国地质,2009,36(3):594-622.
XIAO Qing-hui,DENG Jin-fu,QIU Rui-zhao,et al.A Preliminary Study of the Relationship Between Grani-toids and the Growth of Continental Crust:A Case Study of the Formation of Key Orogen Granitoids in China[J].Geology in China,2009,36(3):594-622.
[79] SALTERS V J M,HART S R.The Mantle Sources of Ocean Ridges,Islands and Arcs:The Hf-isotope Connection[J].Earth and Planetary Science Letters,1991,104(2/3/4):364-380.
[80] PEARCE J A,HARRIS N B W,TINDLE A G.Trace Element Discrimination Diagrams for the Tectonic Interpretation of Granitic Rocks[J].Journal of Petrology,1984,25(4):956-983.

Memo

Memo:
-
Last Update: 2020-09-20