ISSN 1009-6248CN 61-1149/P Bimonthly

Supervisor:China Geological Survey

Sponsored by:XI'an Center of China Geological Survey
Geological Society of China

    • The Core Journals of China
    • The Key Magazine of China Technology
    • CSCD Included Journals
    • Scopus Included Journals
Advance Search
ZHAO Jianan, XU Zhiqin. Gamaleegrad Intermediate Intrusive Rock and Its Geotectonic Significance in the Taxkorgan Region of Western Kunlun Orogenic Belt,Xinjiang[J]. Northwestern Geology, 2017, 50(2): 1-15.
Citation: ZHAO Jianan, XU Zhiqin. Gamaleegrad Intermediate Intrusive Rock and Its Geotectonic Significance in the Taxkorgan Region of Western Kunlun Orogenic Belt,Xinjiang[J]. Northwestern Geology, 2017, 50(2): 1-15.

Gamaleegrad Intermediate Intrusive Rock and Its Geotectonic Significance in the Taxkorgan Region of Western Kunlun Orogenic Belt,Xinjiang

More Information
  • Received Date: January 09, 2017
  • Revised Date: February 27, 2017
  • Available Online: July 28, 2022
  • Published Date: June 04, 2017
  • Gamaleegrad intermediate intrusive rock, located at the southwestern margin of the Tarim Block and the northeast edge of Karakoram continental margin, is composed of calc-alkaline monzogranite series and alkaline granite series, which were formed between late Cambrian and early Ordovician.Based on geochemical analysis, the main elements and trace elements of Gamaleegrad intrusive rock have been studied in detail, as well as the tectonic setting of the intrusive sequence and geodynamic model between plates around the intrusive sequence have been discussed.The results show that the Gamaleegrad intermediate intrusive rock is a combination of monzogranite-granite (MG-G), which is mixed with sub-neutral granitic magma (high Sr, Zr and low Rb) that experienced the crustal remelting in the evolutionary process of intrusive sequence.It mainly belongs to I-type granites, which was formed in continental backarc extensional basin under the condition of subduction collision.Based on physical environment and tectonic setting in the course of magmatic evolution, it is speculated that the formation of these intrusive rock is closely related to subduction collision of Kuda oceanic crust towards Tarim ancient block, indicating the disappearance of Kuda Ocean and the formation of back-arc spreading granite.Meanwhile, it means that the continent-continent collision had taken place between Tarim ancient block and Qaidam ancient block, indicating that both of them were finally converged into Rodinia supercontinent.
  • 崔春龙, 范飞鹏, 李源, 等.西昆仑北坡恰尔隆一带花岗岩类地球化学特征及构造背景初论[J].西南科技大学学报, 2009, 24(1):48-55.
    CUI Chunlong, FAN Feipeng, LI Yuan, et al.Geochemical characteristics of granitoid in the north slope of the West Kunlun and its tectonic setting[J].Journal of Southwest University of Science and Technology, 2009, 24(1):48-55.
    董永观, 郭坤一, 廖圣兵, 等.新疆西昆仑科库西里克铅锌矿床地质及元素地球化学特征[J].地质学报, 2007, 80(11):1730-1738.
    DONG Yongguan, GUO Kunyi, LIAO Shengbing, et al.Geological and geochemical characteristics of lead-zinc deposit of the West Kunlun, Xinjing[J].Acta Geologica Sinica, 2007, 80(11):1730-1738.
    董永观, 郭坤一, 肖惠良, 等.西昆仑地区成矿远景[J].中国地质, 2003, 30(2):173-178.
    DONG Yongguan, GUO Kunyi, XIAO Huiliang, et al.Mineralization prospective of West Kunlun[J].Chinese Geology, 2003, 30(2):173-178 (in Chinese with English abstract).
    方锡廉, 汪玉珍.西昆仑山加里东期花岗岩类浅识[J].新疆地质, 1990, 8(2):153-158.
    FAN Xilian, WANG Yuzhen.Review:Caledonian granitoids in West Kunlun[J].Xinjiang Geology, 1990, 8(2):153-158.
    姜春发.昆仑开合构造[M].北京:地质出版社, 1993, 58-100.
    JIANG Chunfa.Opening-closing Tectonics of Kunlun[M].Beijing:Geological Press, 1993, 58-100.
    姜耀辉, 周珣若, 芮行健, 等.西昆仑造山带花岗岩岩石系列及成因类型[J].地质学报, 2001, 75(1):144-155.
    JIANG Yaohui, ZHOU Xunruo, RUI Xingjian, et al.Series and genesis type of granite of West Kunlun orogenic belt[J].Acta Geologica Sinica, 2001, 75(1):144-155.
    李献华, 李武显, 李正祥.再论南岭燕山早期花岗岩的成因类型与构造意义[J].科学通报, 2007, 52(9):981 -991.
    LI Xianhua, LI Wuxian, LI Zhengxang.Genesis type and tectonic significance of the early Yanshan granites in the Nanling[J].Chinese Science Bulletin, 2007, 52(9):981 -991.
    刘伟新, 丁道桂, 王道轩, 等.西昆仑造山带花岗岩的地质特征及其构造意义[M].北京:地质出版社, 1996.
    LIU Weixin, DING Daogui, WANG Daoxuan, et al.Geological Characteristics of Granite of The West Kunlun Orogenic Belt and Its Tectonic Significance[M].Beijing:Geological Press, 1996.
    鲁新便, 何发岐, 赵洪生.塔里木盆地西南缘构造带的地球物理特征、构造及其演化[J].石油物探, 1997, 36(1):43-52.
    LU Xinbian, HE Faqi, ZHAO Hongsheng.The geophysical feature, structure, and evolution of the tectonic belt in the southwest margin of the Tarim basin[J].Geophysical Prospecting for Petrole, 1997, 36(1):43-52.
    刘学锋, 肖安成.塔里木盆地西南缘构造形变特征[J].江汉石油学院学报, 1996, 18(2):19-24.
    LIU Xuefeng, XIAO Ancheng.Structural deformation characteristics of southwestern margin in Tarim Basin[J].Journal of Jianghan Petroleum Institute, 1996, 18(2):19-24.
    潘裕生.青藏高原第五缝合带的发现与论证[J].地球物理学报, 1994, 37(2):184-192.
    PAN Yusheng.The discovery and demonstration of fifth suture zone in Qinghai-Tibet Plateau[J].Chinese Journal of Geophysics, 1994, 37(2):184-192.
    彭头平, 席先武, 王岳军,等.湘东北早中生代花岗闪长岩地球化学特征及其构造意义[J].大地构造与成矿学, 2004, 28(3):287-296.
    PENG Touping, XI xianwu, WANG Yuejun, et al.Geochemical characteristics of the early Mesozoic granodiorites and their tectonic implications[J].Geotectonica Et Metallogenia, 2004, 28(3):287-296.
    卜文瑞, 王廷印, 马亚杰.华北克拉通北缘西段中元古代花岗岩类的特征及其形成构造环境[J].岩石学报, 2001, 17(4):609-616.
    BU Wenrui, WANG Tingyin, MA Yajie.Characteristics of Mesoproterozoic granitoids of the western part of northern margin of the North China Craton and its tectonic environment[J].Acta Petrologica Sinica, 2001, 17 (4):609-616.
    曲国胜, 李亦纲, 李岩峰, 等.塔里木盆地西南前陆构造分段及其成因[J].中国科学:D 辑, 2005, 35(3):193-202.
    QU Guosheng, LI Yigang, LI Yanfeng, et al.Foreland tectonic segmentation and geneses of the southwastern Tarim Basin[J].Science in China,Ser.D, 2005, 35(3):193-202 (in Chinese with English abstract).
    曲国胜, 李亦纲, 张宁, 等.塔里木西南缘 (齐姆根弧) 前陆构造及形成机理[J].地质论评, 2004, 50(6):567-576.
    QU Guosheng, LI Yigang, ZHANG Ning, et al.A Study on the Foreland Structure of the Qimugen Arc in Southwest Tarim and Its Genetic Mechanism[J].Geological Review,2004, 50 (6):567-576,588.
    孙宝生, 刘增仁.塔里木西南喀什凹陷几个地质问题的新认识[J].新疆地质, 2003, 21(1):78-84.
    SUN Baosheng, LIU Zengren, WANG Zhaoming.New knowledge on geology of Kashi Depression in Southwest Tarim[J].Xinjiang Geology, 2003,21 (1):78-84.
    王光杰, 滕吉文, 张中杰.中国华南大陆及陆缘地带的大地构造基本格局[J].地球物理学进展, 2000, 15(3):25-43.
    WANG Guangjie, TENG Jiwen, ZHANG Zhongjie.Tectonic basic pattern of South China and its continental margin[J].Progress in Geophysics, 2000, 15(3):25-43.
    巫建华, 刘帅.大地构造学概论与中国大地构造学纲要[M].北京:地质出版社, 2008.
    WU Jianhua, LIU Shuai.Introduction to Geotectonics and Outline of Chinese Earth Tectonics[M].Beijiang:Geological Press, 2008.
    伍致中, 刘东海.塔里木盆地西南坳陷的形成演化[J].新疆石油地质, 1996, 17(3):211-218.
    WU Zhizhong, LIU Donghai.The formation and evolution of Southwest Depression of Tarim Basin[J].Xinjiang petroleum Geology, 1996, 17(3):211-218.
    杨克明.论西昆仑大陆边缘构造演化及塔里木西南盆地类型[J].地质论评, 1994, 40(1):9-18.
    YANG Keming.The formation and evolution of the Western Kunlun continental margin[J].Geological Review, 1994, 40(1):9-18.
    姚卫江, 陈文利, 肖燕, 等.塔里木盆地西南坳陷周边山前的典型构造模式建立[J].新疆地质, 2009 (S1):47-50.
    YAO Weijiang, CHEN Wenli, XIAO Yan, et al.Establishment of typical structural models for piedmont areas surrounding southwestern Tarim Depression[J].Xinjiang Geology, 2009(S1):47-55.
    张传林, 杨淳, 沈加林, 等.西昆仑北缘新元古代片麻状花岗岩锆石SHRIMP 年龄及其意义[J].地质论评, 2003, 3:239-244.
    ZHANG Chuanlin, YANG Chun, SHEN Jialin, et al.The zircon SHRIMP age of Late Proterozoic gneissic granite of West Kunlun and its significance[J].Geological Review, 2003, 3:239-244.
    张传林, 陆松年, 于海锋, 等.塔里木西南缘中元古代末期大陆汇聚及新元古代大陆裂解[A].2004 年全国岩石学与地球动力学研讨会论文摘要集[C], 2004.
    ZHANG Chuanlin, LU Songnian, YU Haifeng, et al.Proterozoic continental convergence and Neoproterozoic continental breakup in the southwest margin of Tarim[A].The National Petrology and the Earth Dynamics Conference in 2004[C],2004.
    张旗, 王焰, 李承东, 等.花岗岩的 Sr-Yb 分类及其地质意义[J].岩石学报, 2006, 22(9):2249-2269.
    ZHANG Qi, WANG Yan, LI Chengdong, et al.Granite classification on the basis of Sr and Yb contents and its implications[J].Acta Petrologica Sinica, 2006, 22(9):2249-2269.
    张旗, 金惟俊, 李承东, 等.花岗岩与地壳厚度关系探讨[J].大地构造与成矿学, 2011, 35(2):259-269.
    ZHANG Qi, JIN Weijun, LI Chengdong, et al.Granitic rocks and their formation depth in the crust[J].Geotectonica Et Metallogenia, 2011, 35(2):259-269.
    赵佳楠, 刘正军.新疆西昆仑造山带北缘中元古代帕什托克闪长岩侵入序列及其地质意义[J].中国地质, 2014, 41(1):92-107.
    ZHAO Jianan, LIU Zhengjun.Mesoproterozoic Pashtok diorite intrusive sequence on the northern margin of West Kunlun orogenic belt in Xinjiang and its geological implications[J].Geology in China, 2014, 41(1):92-107.
    BARKER F.Trondhjemite:definition, environment and hypotheses of origin.Elsevier[J].Amsterdam, 1979, 1-12.
    CHAPPELL B W and WHITE A J R.Two contrasting granite types[J].Pacific Geology, 1974, 8(2):173-174.
    CONDIE K C and HUNTER D R.Trace element geochemistry of Archean granitic rocks from the Barberton region, South Africa[J].Earth and Planetary Science Letters, 1976, 29(2):389-400.
    FROSTB R, BARNES C G, COLLINS W J,et al.A geochemical classification for granitic rocks[J].Journal of Petrology, 2001, 42(11):2033-2048.
    LAMEYREJ and BOWDEN P.Plutonic rock types series:discrimination of various granitoid series and related rocks[J].Journal of Volcanology and Geothermal Research, 1982, 14(1):169-186.
    LOISELLEM C and WONES D R.Characteristics and origin of anorogenic granites[J].Geological Society of America Abstracts with Programs, 1979, 11(7):468.
    MAITRER W, STRECKEISEN A, ZANETTIN B,et al.A classification of igneous rocks and glossary of terms:Recommendations of the International Union of Geological Sciences Subcommission on the Systematics of igneous rocks[J].Oxford Blackwell, 1989, 193.
    MANIAR P D and PICCOLI P M.Tectonic discrimination of granitoids[J].Geological Society of America Bulletin, 1989, 101(5):635-643.
    MATTE P, TAPPONNIER P, ARNAUD N, et al.Tectonics of Western Tibet, between the Tarim and the Indus[J].Earth and Planetary Science Letters, 1996,142(3):311-330.
    MIDDLEMOSTE A K.Magmas and magmatic rocks:An introduction to igneous petrology[J].New York:Longman, 1985, 1(1):266.
    PEARCE J A, HARRIS N B W and TINDLE A G.Trace element discrimination diagrams for the tectonic interpretation of granitic rocks[J].Journal of Petrology, 1984, 25(4):956-983.
    ROCHE H, LETERRIER J, GRANDCLAUDE P et al.A classification of volcanic and plutonic rocks using R1-R2 diagram and major-element analyses:Its relationships with current nomenclature[J].Chemical Geology, 1980, 29(1):183-210.
    SUNS S and Mcdonough W F.Chemical and isotopic systematics of oceanic basalts:implications for mantle composition and processes[J].Geological Society, London, Special Publications, 1989, 42(1):313-345.
    WICKHAM S M and LI Z L.Granite for instructions tectonic setting[J].Geological Science and Technology Information, 1989, 4:20.
    ZHANGChuanlin, DONG Yongguan, ZHAO Yu,et al.Geochemistry of Mesoproterozoic volcanic rocks in West Kunlun:evidence for the plate tectonic evolution[J].Acta Geologica Sinica, 2003, 78:532-542.
  • Related Articles

Catalog

    Article views (2810) PDF downloads (3540) Cited by()

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return