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Volume 42 Issue 2
Mar.  2020
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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2020  >  42(2): 172-176
HE Guangyu, GU Yi, ZHAO Yongqiang, YAO Zewei, ZHENG Xiaoli, XIAO Sidong, HUANG Jiwen, JIA Cunshan, ZHOU Yushuang. Evidence of two-stage strike-slip structural deformation of Shaya Uplift, northern Tarim Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2020, 42(2): 172-176. doi: 10.11781/sysydz202002172
Citation: HE Guangyu, GU Yi, ZHAO Yongqiang, YAO Zewei, ZHENG Xiaoli, XIAO Sidong, HUANG Jiwen, JIA Cunshan, ZHOU Yushuang. Evidence of two-stage strike-slip structural deformation of Shaya Uplift, northern Tarim Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2020, 42(2): 172-176. doi: 10.11781/sysydz202002172
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Evidence of two-stage strike-slip structural deformation of Shaya Uplift, northern Tarim Basin

doi: 10.11781/sysydz202002172
  • 1.

    School of Earth Sciences, Zhejiang University, Hangzhou, Zhejiang 310027, China

  • 2.

    Wuxi Research Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214126, China

  • 3.

    Ocean College, Zhejiang University, Zhoushan, Zhejiang 316021, China

  • 4.

    BGP Inc, CNPC, Korla, Xinjiang 841000, China

  • 5.

    Zhejiang GOGA Energy Technology Company, Hangzhou, Zhejiang 310023, China

  • Received Date: 2019-12-07
  • Rev Recd Date: 2020-02-07
  • Publish Date: 2020-03-28
    Abstract
  • The Shaya Uplift, an important structural belt in the northern Tarim Basin, northwestern China, has been regarded as a thrust belt. However, this recognition is not only incompatible with the flower structures on the seismic profiles, but also contradictory with the fault distribution in a broom or trailer mode in plan view. High-resolution 3D seismic profiles indicate that a two-stage strike-slip structural deformation happened in the Shaya Uplift. The first is from the Late Caledonian to the Indosinian, in which transpressional deformation occurred and a huge positive flower structure was thus formed in the deeper part, and strata were eroded because of the structural uplifting. The second is during the Himalayan, in which a negative inverted/transtensional deformation occurred and a negative flower structure was formed in the shallower part. These results indicate that it is not a uniform tectonic-sedimentary environment in the northern Tarim because of the Shaya Uplift barrier and that the Late Caledonian and the Early Himalayan may be two important structural transformation periods.

     

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    • References(21)
  • [1]
    代寒松. 塔里木盆地沙雅隆起构造特征及含油气条件研究[D]. 成都: 成都理工大学, 2007: 18-31.

    DAI Hansong. The analysis of tectonic character and favored condition of oil-gas gathering in Shaya Uplift of Tarim Basin[D]. Chengdu: Chengdu University of Technology, 2007: 18-31.
    [2]
    王峰. 塔北隆起东部地质结构与构造演化[D]. 北京: 中国地质大学(北京), 2018: 46-59.

    WANG Feng. Geological architecture and tectonic evolution in the eastern segment of the Tabei Uplift[D]. Beijing: China University of Geosciences, 2018: 46-59.
    [3]
    何磊. 塔北隆起西段构造演化及其控油气作用[D]. 北京: 中国地质大学(北京), 2017: 85-96.

    HE Lei. Tectonic evolution and its control on hydrocarbon accumulation of western segment of the North-Tarim Uplift[D]. Beijing: China University of Geosciences, 2017: 85-96.
    [4]
    徐宏节, 吴亚军. 雅克拉断凸及周缘地区的复合圈闭特征[J]. 天然气工业, 2004, 24(3): 26-28. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG200403008.htm

    XU Hongjie, WU Yajun. Combination trap characteristics of Yakela Fault Arch and its surrounding areas[J]. Natural Gas Industry, 2004, 24(3): 26-28. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG200403008.htm
    [5]
    崔海峰. 塔北隆起西段构造特征与油气成藏[D]. 成都: 成都理工大学, 2011: 13-39.

    CUI Haifeng. Tectonic features and reservoir accumulation in the west Tabei Uplift[D]. Chengdu: Chengdu University of Techno-logy, 2011: 13-39.
    [6]
    张宁宁, 侯连华, 何登发, 等. 塔北隆起-库车坳陷西段差异构造变形特征及其控制因素[J]. 地质通报, 2017, 36(4): 616-623. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201704015.htm

    ZHANG Ningning, HOU Lianhua, HE Dengfa, et al. Structural characteristics and controlling factors in western Tabei Uplift-Kuqa Depression area, Tarim Basin[J]. Geological Bulletin of China, 2017, 36(4): 616-623. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201704015.htm
    [7]
    安传杰. 塔北隆起轴部断裂系统及成因机制[D]. 北京: 中国地质大学(北京), 2017: 52-85.

    AN Chuanjie. Fault system and mechanism of axial area in North Tarim[D]. Beijing: China University of Geosciences, 2017: 52-85.
    [8]
    何文渊, 李江海, 钱祥麟, 等. 塔里木盆地北部隆起负反转构造成因机制探讨[J]. 地质科学, 2017, 36(2): 234-240. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKX200102013.htm

    HE Wenyuan, LI Jianghai, QIAN Xianglin, et al. Mechanism of negative inversion-structuring in North Tarim Uplift[J]. Chinese Journal of Geology, 2017, 36(2): 234-240. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKX200102013.htm
    [9]
    张师本, 倪寓南, 龚福华, 等. 塔里木盆地周缘地层考察指南[M]. 北京: 石油工业出版社, 2003: 9-123.

    ZHANG Shiben, NI Yu'nan, GONG Fuhua, et al. A guide to the stratigraphic investigation on the periphery of the Tarim Basin[M]. Beijing: Petroleum Industry Press, 2003: 9-123.
    [10]
    储呈林. 塔北隆起南斜坡上泥盆统-石炭系层序结构、沉积演化及其控制因素[D]. 北京: 中国地质大学(北京), 2011: 84-86.

    CHU Chenglin. Sequence stratigraphy, sedimentary evolution and its controlling factors of Upper Devonian-Carboniferous in the south slope of the Tabei Uplift[D]. Beijing: China University of Geosciences, 2011: 84-86.
    [11]
    WINDLEY B F, ALLEN M B, ZHANG C, et al. Paleozoic accretion and Cenozoic redeformation of the Chinese Tie Shan Range, central Asia[J]. Geology, 1990, 18(2): 128-131. doi: 10.1130/0091-7613(1990)018<0128:PAACRO>2.3.CO;2
    [12]
    MATTERN F, SCHNEIDER W. Suturing of the Proto-and Paleo-Tethys oceans in the western Kunlun (Xinjiang, China)[J]. Journal of Asian Earth Sciences, 2000, 18(6): 637-650. doi: 10.1016/S1367-9120(00)00011-0
    [13]
    何治亮, 罗传荣, 龚铭. 塔里木多旋回盆地与复式油气系统[M]. 武汉: 中国地质大学出版社, 2001: 8-18.

    HE Zhiliang, LUO Chuanrong, GONG Ming. The multicyclic evolution and multiple petroleum system of Tarim Basin[M]. Wuhan: China University of Geoscience Press, 2001: 8-18.
    [14]
    彭莉. 塔北隆起南斜坡志留纪古构造地貌及沉积演化[D]. 北京: 中国地质大学(北京), 2010: 64-86.

    PENG Li. The Evolution of Silurian structural paleogemorphology and sedimentology, the south slope of Tabei Uplift, Tarim Basin[D]. Beijing: China University of Geosciences, 2010: 64-86.
    [15]
    CHEN Chuming, LU Huadu, JIA Dong, et al. Closing history of the southern Tianshan oceanic basin, Western China: an oblique collisional orogen[J]. Tectonophysics, 1999, 302(1/2): 23-40.
    [16]
    WANG Zhihong. Tectonic evolution of the Western Kunlun Orogenic Belt, Western China[J]. Journal of Asian Earth Sciences, 2004, 24(2): 153-161. doi: 10.1016/j.jseaes.2003.10.007
    [17]
    郭令智, 施央申, 卢华复, 等. 印藏碰撞的两种远距离效应[M]//李清波, 戴金星, 刘如琦, 等. 现代地质学研究文集(上). 南京: 南京大学出版社, 1992: 1-7.

    GUO Linzhi, SHI Yangshen, LU Huafu, et al. Two long-distance effects from the collision between India and Tibet[M]//LI Qingbo, DAI Jinxing, LIU Ruqi, et al. The proceedings of the modern geology (part 1). Nanjing: Nanjing University Press, 1992: 1-7.
    [18]
    MOLNAR P, TAPPONNIER P. Cenozoic tectonics of Asia: effects of a continental collision[J]. Science, 1975, 189(4201): 419-426. doi: 10.1126/science.189.4201.419
    [19]
    HENDRIX M S, DUMITRU T A, GRAHAM S A. Late Oligocene-Early Miocene unroofing in the Chinese Tianshan: an early effect of the India-Asia collision[J]. Geology, 1994, 22(6): 487-490.
    [20]
    SOBEL E R, DUMITRU T A. Thrusting and exhumation around the margins of the western Tarim Basin during the India-Asia collision[J]. Journal of Geophysical Research: Solid Earth, 1997, 102(B3): 5043-5063.
    [21]
    王燮培, 费琪. 石油构造样式分析[M]. 武汉: 中国地质大学出版社, 1988.

    WANG Xipei, FEI Qi. Analysis on petroleum structural styles[M]. Wuhan: China University of Geoscience Press, 1988.
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