GAO Shanlin. Geochemical characteristics and geologic significance of the Lower Jurassic basalt on the western margin of Junggar Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2019, 41(3): 420-426. doi: 10.11781/sysydz201903420
Citation: GAO Shanlin. Geochemical characteristics and geologic significance of the Lower Jurassic basalt on the western margin of Junggar Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2019, 41(3): 420-426. doi: 10.11781/sysydz201903420

Geochemical characteristics and geologic significance of the Lower Jurassic basalt on the western margin of Junggar Basin

doi: 10.11781/sysydz201903420
  • Received Date: 2019-03-13
  • Rev Recd Date: 2019-04-22
  • Publish Date: 2019-05-28
  • The geochemical characteristics of the Lower Jurassic volcanic rocks on the western margin of the Junggar Basin were analyzed. The main, trace and rare earth element data indicate that the rocks are alkaline basalts, enriched with light rare earth elements, large ion lithophile elements and high field strength elements. The trace elements show an ocean island basalt (OIB) distribution model. The basalt magma came from the depleted mantle that was not obviously contaminated by crust, and has the characteristics of continental intraplate rift volcanic rocks related to mantle plume activity. The Tubo-Hami, Dunhuang and other basins in the northwest developed Jurassic basalt of similar genesis with the western Junggar Basin. The basalt formation was related to the rising of regional asthenosphere interface and the thinning of lithosphere, providing dynamic conditions for the formation of extension basin during the early and middle Jurassic. The extension of the Jurassic basin took place earlier in the west and the south, which explained the difference of source rock distribution and hydrocarbon accumulation in the basin.

     

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  • [1]
    马小伟,朱传真,林玉祥,等.准噶尔盆地温压系统演化与油气远源成藏[J].石油实验地质,2017,39(4):467-476.

    MA Xiaowei,ZHU Chuanzhen,LIN Yuxiang,et al.Evolution of the temperature-pressure system and far-source hydrocarbon accumulation in Junggar Basin[J].Petroleum Geology and Experiment,2017,39(4):467-476.
    [2]
    刘和甫,汪泽成,熊保贤,等.中国中西部中、新生代前陆盆地与挤压造山带耦合分析[J].地学前缘,2000,7(3):55-72.

    LIU Hefu,WANG Zecheng,XIONG Baoxian,et al.Coupling ana-lysis of Mesozoic-Cenozoic foreland basin and mountain system in central and western China[J].Earth Science Frontiers,2000,7(3):55-72.
    [3]
    李忠权,陈更生,张寿庭.新疆准噶尔盆地南缘拉张伸展动力学环境的探讨[J].高校地质学报,1998,4(1):73-78.

    LI Zhongquan,CHEN Gengsheng,ZHANG Shouting.Discussion on the extensional dynamic setting in the south border of Junggar Basin,Xinjiang,China[J].Geological Journal of China Universities,1998,4(1):73-78.
    [4]
    蔡忠贤,陈发景,贾振远.准噶尔盆地的类型和构造演化[J].地学前缘,2000,7(4):431-440.

    CAI Zhongxian,CHEN Fajing,JIA Zhenyuan.Types and tectonic evolution of Junger Basin[J].Earth Science Frontiers,2000,7(4):431-440.
    [5]
    石好果.准噶尔盆地腹部阜康深凹带侏罗系成藏规律[J].石油实验地质,2017,39(2):238-246.

    SHI Haoguo.Jurassic reservoir development in Fukang Deep Sag,Central Junggar Basin[J].Petroleum Geology and Experiment,2017,39(2):238-246.
    [6]
    中国科学院地学部,新疆石油管理局.准噶尔盆地形成演化与油气形成[M].北京:科学出版社,1989:29-30. Department of Geology of Chinese Academy of Sciences,Xinjiang Petroleum Administration.Evolution and hydrocarbon formation in Junggar Basin[M].Beijing:Science Press,1989:29-30.
    [7]
    WINCHESTER J A,FLOYD P A.Geochemical discrimination of different magma series and their differentiation products using immobile elements[J].Chemical Geology,1997,20:325-343.
    [8]
    王岳军,廖超林,范蔚茗,等.赣中地区早中生代OIB碱性玄武岩的厘定及构造意义[J].地球化学,2004,33(2):109-117.

    WANG Yuejun,LIAO Chaolin,FAN Weiming,et al.Early Mesozoic OIB-type alkaline basalt in central Jiangxi Province and its tectonic implications[J].Geochimica,2004,33(2):109-117.
    [9]
    董云鹏,周鼎武,张国伟,等.秦岭造山带南缘早古生代基性火山岩地球化学特征及其大地构造意义[J].地球化学,1998,27(5):432-441.

    DONG Yunpeng,ZHOU Dingwu,ZHANG Guowei,et al.Geoche-mistry of the Caledonian basin volcanic rocks in the south margin of Qinling Orogenic Belt and their tectonic imolications[J].Geochi-mica,1998,27(5):432-441.
    [10]
    MASUDA A,NAKAMURA N,TANAKA T.Fine structures of mutually normalized rare-earth patterns of chondrites[J].Geochimica et Cosmochimica Acta,1973,37(2):239-248.
    [11]
    AJAJI T,WEIS D,GIRET A,et al.Coeval potassic and sodic calc-alkaline series in the post-collisional Hercynian Tanncherfi intrusive complex,northeastern Morocco:geochemical,isotopic and geochronological evidence[J].Lithos,1998,45(1/4):371-393.
    [12]
    李昌年.火成岩微量元素岩石学[M].武汉:中国地质大学出版社,1992:85-113. LI Changnian.Trace element petrology of igneous rocks[M].Wuhan:China University of Geosciences Press,1992:85-113.
    [13]
    SUN S S,MC DONOUGH W F.Chemical and isotopic systema-tics of oceanic basalts:implications for mantle composition and processes[J].Geological Society,London,Special Publications,1989,42(1):313-345.
    [14]
    HOFMANN A W.Chemical differentiation of the earth:the relationship between mantle,continental crust,and oceanic crust[J].Earth and Planetary Science Letter,1988,90(3):297-314.
    [15]
    WOOD D A.The application of a Th-Hf-Ta diagram to problems of tectonomagmatic classification and to establishing the nature of crustal contamination of basaltic lavas of the British Tertiary volcanic province[J].Earth and Planetary Science Letters,1980,50(1):11-30.
    [16]
    吴昌志,顾连兴,任作伟,等.辽河盆地沙三期火山-侵入岩地球化学与岩石成因[J].岩石学报,2004,20(3):545-556.

    WU Changzhi,GU Lianxing,REN Zuowei,et al.Geochemistry and petrogenesis of Eocene volcanic-intrusive rocks in Liaohe Basin,northeastern China[J].Acta Petrologica Sinica,2004,20(3):545-556.
    [17]
    贾大成,丘学林,胡瑞忠,等.北部湾玄武岩地幔源区性质的地球化学示踪及其构造环境[J].热带海洋学报,2003,22(2):30-39.

    JIA Dacheng,QIU Xuelin,HU Ruizhong,et al.Geochemical nature of mantle reservoirs and tectonic setting of basalts in Beibu Gulf and its adjacent region[J].Journal of Tropical Oceanography,2003,22(2):30-39.
    [18]
    汪云亮,张成江,修淑芝.玄武岩类形成的大地构造环境的Th/Hf-Ta/Hf图解判别[J].岩石学报,2001,17(3):413-421.

    WANG Yunliang,ZHANG Chengjiang,XIU Shuzhi.Th/Hf-Ta/Hf identification of tectonic setting of basalts[J].Acta Petrologica Sinica,2001,17(3):413-421.
    [19]
    王登红,李建康,刘峰,等.地幔柱研究中几个问题的探讨及其找矿意义[J].地球学报,2004,25(5):489-494.

    WANG Denghong,LI Jiankang,LIU Feng,et al.Some problems related to mantle plume and their significance in ore prospecting[J].Acta Geoscientica Sinica,2004,25(5):489-494.
    [20]
    肖龙,徐义刚,梅厚钧,等.云南金平晚二叠纪玄武岩特征及其与峨眉地幔柱关系:地球化学证据[J].岩石学报,2003,19(1):38-48.

    XIAO Long,XU Yigang,MEI Houjun,et al.Late Permian flood basalts at Jinping area and its relation to Emei mantle plume:geochemical evidences[J].Acta Petrologica Sinica,2003,19(1):38-48.
    [21]
    张志诚,郭召杰,韩作振.敦煌盆地中侏罗世火山岩的地球化学特征及其地质意义[J].北京大学学报(自然科学版),1998,34(1):72-79. ZHANG Zhicheng,GUO Zhaojie,HAN Zuozhen.Geochemistry and geological significance of the Mid Jurassic volcanic rocks in Dunhuang Basin[J].Acta Scicentiarum Naturalum Universitis Pekinesis,1998,34(1):72-79.
    [22]
    崔俊,陈登钱,姚熙海.柴达木盆地冷湖地区侏罗纪火山活动浅析[J].青海石油,2004,22(1):17-20.

    CUI Jun,CHEN Dengqian,YAO Xihai.A brief analysis of Jurassic volcanic activities in Lenghu area of Qaidam[J].Qinghai Petro-leum,2004,22(1):17-20.
    [23]
    李荣社,杨永成,孟勇.青藏高原1:25万区域地质调查主要成果和进展综述(北区)[J].地质通报,2004,23(5-6):421-426. LI Rongshe,YANG Yongcheng,MENG Yong.Main results and progress in 1:250000 regional geological survey of the northern Qinghai-Tibet Plateau[J].Geological Bulletin of China,2004,23(5-6):421-426.
    [24]
    朱云海,朱耀生,林启祥,等.东昆仑造山带海德乌拉一带早侏罗世火山岩特征及其构造意义[J].地球科学(中国地质大学学报),2003,28(6):653-659. ZHU Yunhai,ZHU Yaosheng,LIN Qixiang,et al.Characteristics of Early Jurassic volcanic rocks and their tectonic significance in Haidewula,East Kunlun Orogenic Belt,Qinghai Province[J].Earth Science (Journal of China University of Geosciences),2003,28(6):653-659.
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