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柴达木盆地西部阿拉尔断裂新生代构造变形特征及意义

魏岩岩, 吴磊, 周道卿, 肖安成, 黄凯. 2021. 柴达木盆地西部阿拉尔断裂新生代构造变形特征及意义. 物探与化探, 45(5): 1171-1178. doi: 10.11720/wtyht.2021.0091
引用本文: 魏岩岩, 吴磊, 周道卿, 肖安成, 黄凯. 2021. 柴达木盆地西部阿拉尔断裂新生代构造变形特征及意义. 物探与化探, 45(5): 1171-1178. doi: 10.11720/wtyht.2021.0091
WEI Yan-Yan, WU Lei, ZHOU Dao-Qing, XIAO An-Cheng, HUANG Kai. 2021. Cenozoic tectonic deformation characteristics of Alar fault in southwestern Qaidam Basin and their significance. Geophysical and Geochemical Exploration, 45(5): 1171-1178. doi: 10.11720/wtyht.2021.0091
Citation: WEI Yan-Yan, WU Lei, ZHOU Dao-Qing, XIAO An-Cheng, HUANG Kai. 2021. Cenozoic tectonic deformation characteristics of Alar fault in southwestern Qaidam Basin and their significance. Geophysical and Geochemical Exploration, 45(5): 1171-1178. doi: 10.11720/wtyht.2021.0091

柴达木盆地西部阿拉尔断裂新生代构造变形特征及意义

  • 基金项目:

    国家自然科学基金面上项目(41972218)

    中国地质调查局地质调查项目

    银额盆地及外围航空物探调查(DD20190025)

详细信息
    作者简介: 魏岩岩(1989-),女,工程师,现主要从事盆地分析、地震解释、航空重磁解释等工作。Email: hbweiyanyan@163.com
  • 中图分类号: P631.4

Cenozoic tectonic deformation characteristics of Alar fault in southwestern Qaidam Basin and their significance

  • 依据二维、三维地震资料,精细分析位于柴达木盆地西南部的阿拉尔断裂的几何学特征、水平缩短量及活动时间等,并探讨了其整个新生代的运动学特征、形成机制和油气地质意义。结果表明,阿拉尔断裂平面上可分为NWW走向的西段和近SN走向的东段,两段近于垂直;剖面上,其西段倾向南,倾角相对较小,而东段倾向西,断面近乎直立。阿拉尔断裂自新生代初期开始活动,西段以逆冲为主,水平缩短量和竖直抬升量均达到3 km以上,走滑量约为1 km;东段以右旋走滑为主,水平缩短量和竖直抬升量为1 km左右,走滑量达到3 km。阿拉尔断裂的形成和活动受南侧祁漫塔格造山带向北挤压和西侧阿尔金左旋走滑断裂的共同影响,柴西南地区断裂活动与油气形成具有良好的时空匹配关系,对形成油气藏具有重要意义。
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  • [1]

    戴俊生, 曹代勇. 柴达木盆地新生代构造样式的演化特点[J]. 地质论评, 2000, 46(5):455-460.

    [2]

    Dai J S, Cao D Y. Evolution characteristics of Cenozoic structural style in the Qaidam Basin[J]. Geological Review, 2000, 46(5):455-460.

    [3]

    汤良杰, 金之钧, 戴俊生, 等. 柴达木盆地及相邻造山带区域断裂系统[J]. 地球科学, 2002, 27(6):676-682.

    [4]

    Tang L J, Jin Z Y, Dai J S, et al. Regional fault systems of Qaidam Basin and adjacent Orogenic belts[J]. Earth Science, 2002, 27(6):676-682.

    [5]

    付锁堂, 关平, 张道伟. 柴达木盆地近期勘探工作思考[J]. 天然气地球科学, 2012, 23(5):813-819.

    [6]

    Fu S T, Guan P, Zhang D W. Consideration about recent oil and gas exploration of Qaidam Basin[J]. Natural Gas Geoscience, 2012, 23(5):813-819.

    [7]

    关平, 简星. 青藏高原北部新生代构造演化在柴达木盆地中的沉积记录[J]. 沉积学报, 2013, 31(5):824-833.

    [8]

    Guan P, Jian X. The Cenozoic sedimentary record in Qaidam Basin and its implications for tectonic evolution of the Northern Tibetan Plateau[J]. Acta Sedimentologica Sinica, 2013, 31(5):824-833.

    [9]

    Zhou J, Xu F, Wang T, et al. Cenozoic deformation history of the Qaidam Basin,NW China:Results from cross-section restoration and implications for Qinghai-Tibet Plateau tectonics[J]. Earth and Planetary Science Letters, 2006, 243(1-2):195-210.

    [10]

    Wei Y, Xiao A, Wu L, et al. Temporal and spatial patterns of Cenozoic deformation across the Qaidam Basin,Northern Tibetan Plateau[J]. Terra Nova, 2016, 28(6):409-418.

    [11]

    Wu L, Xiao A, Ma D, et al. Cenozoic fault systems in southwest Qaidam Basin, northeastern Tibetan Plateau:Geometry,temporal development,and significance for hydrocarbon accumulation[J]. AAPG Bulletin, 2014, 98(6):1213-1234.

    [12]

    崔兴宝. 综合勘探技术在柴达木盆地西部地区的应用[J]. 物探与化探, 2003, 27(3):171-175.

    [13]

    Cui X B. The application of the integrated exploration technique to the western part of qaidam basin[J]. Geophysical and Geochemical Exploration, 2003, 27(3):171-175.

    [14]

    熊业刚, 罗铮, 张启全, 等. 逆掩断裂带正演分析与解释——以英雄岭地区为例[J]. 物探与化探, 2019, 43(3):551-557.

    [15]

    Xiong Y G, Luo Z, Zhang Q Q, et al. Overthrust belt forward analysis and interpretation:A case study of Yingxiongling area[J]. Geophysical and Geochemical Exploration, 2019, 43(3):551-557.

    [16]

    Mao L, Xiao A, Wu L, et al. Cenozoic tectonic and sedimentary evolution of southern Qaidam Basin,NE Tibetan Plateau and its implication for the rejuvenation of Eastern Kunlun Mountains[J]. Science China Earth Sciences, 2014, 57(11):2726-2739.

    [17]

    倪金龙, 汪劲草, 周莉, 等. 中—新生代东昆仑造山带构造事件及柴西南盆地原型研究[J]. 现代地质, 2007, 21(3):505-510.

    [18]

    Ni J L, Wang J C, Zhou L, et al. Study on the Tectonic events of East-Kunlun Orogenic Belt and Prototype about West-South Qaidam Basin during Mesozoic and Cenizoic[J]. Geoscience, 2007, 21(3):505-510.

    [19]

    Xiang C, Fu S, Wang H, et al. Geometry and kinematics of the Arlar strike-slip fault,SW Qaidam basin,China:New insights from 3-D seismic data[J]. Journal of Asian Earth Sciences, 2015, 98:198-208.

    [20]

    方向, 张永庶. 柴达木盆地西部地区新生代沉积与构造演化[J]. 地质与勘探, 2014, 50(1):28-36.

    [21]

    Fang X, Zhang Y S. Cenozoic sediments and tectonic evolution in the western Qaidam basin[J]. Geology and Exploration, 2014, 50(1):28-36.

    [22]

    李兰斌, 孙丽娜, 孙家振, 等. 柴西南地区断裂特征分析[J]. 石油地球物理勘探, 2010, 45(3):443-447.

    [23]

    Li L B, Sun L N, Sun J Z, et al. The fracture characteristic analysis in Southwest area of Qaidam Basin[J]. Oil Geophysical Prospecting, 2010, 45(3):443-447.

    [24]

    Chen W P, Chen C Y, L N A Belek J. Present-day deformation of the Qaidam basin with implications for intra-continental tectonics[J]. Tectonophysics, 1999, 305(1-3):165-181.

    [25]

    Wang Y, Zheng J, Zhang W, et al. Cenozoic uplift of the Tibetan Plateau:Evidence from the tectonic-sedimentary evolution of the western Qaidam Basin[J]. Geoscience Frontiers, 2012, 3(2):175-187.

    [26]

    Wang Y, Nie J, Zhang T, et al. Cenozoic tectonic evolution in the western Qaidam Basin inferred from subsurface data[J]. Geosciences Journal, 2010, 14(4):335-344.

    [27]

    王亚东, 张涛, 迟云平, 等. 柴达木盆地西部地区新生代演化特征与青藏高原隆升[J]. 地学前缘, 2011, 18(3):141-150.

    [28]

    Wang Y D, Zhang T, Chi Y P, et al. Cenozoic uplift of the Tibetan Plateau:Evidence from tectonic-sedimentary evolution of the Western Qaidam Basin[J]. Earth Science Frontiers, 2011, 18(3):141-150.

    [29]

    方向, 江波, 张永庶. 柴达木盆地西部地区断裂构造与油气聚集[J]. 石油与天然气地质, 2006, 27(1):56-61.

    [30]

    Fang X, Jiang B, Zhang Y S. Faulted structure and hydrocarbon accumulation in western Qaidam basin[J]. Oil and Gas Geology, 2006, 27(1):56-61.

    [31]

    Cheng F, Jolivet M, Fu S, et al. Northward growth of the Qimen Tagh Range:A new model accounting for the Late Neogene strike-slip deformation of the SW Qaidam Basin[J]. Tectonophysics, 2014, 632:32-47.

    [32]

    Meng Q R, Fang X. Cenozoic tectonic development of the Qaidam Basin in the northeastern Tibetan Plateau[J]. Geological Society of America Special Papers, 2008, 444:1-24.

    [33]

    Yin A, Dang Y, Zhang M, et al. Cenozoic tectonic evolution of Qaidam basin and its surrounding regions (part 2):Wedge tectonics in southern Qaidam basin and the Eastern Kunlun Range[J]. Geological Society of America Special Papers, 2007, 433:369-390.

    [34]

    Yin A, Dang Y Q, Zhang M, et al. Cenozoic tectonic evolution of the Qaidam basin and its surrounding regions (Part 3):Structural geology,sedimentation,and regional tectonic reconstruction[J]. Geological Society of America Bulletin, 2008, 120(7-8):847-876.

    [35]

    陈海清. 柴达木盆地柴西南三维区岩性地层圈闭识别技术研究[D]. 青岛:中国海洋大学, 2010.

    [36]

    Chen H Q. A research on the techniques for identifying lithologic stratigraphic traps in the Southwest 3D survey of Chaidamu Basin[D]. Qingdao:Ocean University of China, 2010.

    [37]

    Ji J L, Zhang K X, Clift P D, et al. High-resolution magnetostratigraphic study of the Paleogene-Neogene strata in the Northern Qaidam Basin:Implications for the growth of the Northeastern Tibetan Plateau[J]. Gondwana Research, 2017, 46:141-155.

    [38]

    Sun Z, Yang Z, Pei J, et al. Magnetostratigraphy of Paleogene sediments from northern Qaidam Basin,China:Implications for tectonic uplift and block rotation in northern Tibetan plateau[J]. Earth and Planetary Science Letters, 2005, 237(3-4):635-646.

    [39]

    Lu H, Xiong S. Magnetostratigraphy of the Dahonggou section,northern Qaidam Basin and its bearing on Cenozoic tectonic evolution of the Qilian Shan and Altyn Tagh Fault[J]. Earth and Planetary Science Letters, 2009, 288(3-4):539-550.

    [40]

    Fang X, Zhang W, Meng Q, et al. High-resolution magnetostratigraphy of the Neogene Huaitoutala section in the eastern Qaidam Basin on the NE Tibetan Plateau,Qinghai Province,China and its implication on tectonic uplift of the NE Tibetan Plateau[J]. Earth and Planetary Science Letters, 2007, 258(1-2):293-306.

    [41]

    徐波. 运用地震属性研究柴达木盆地早新生代断裂特征[D]. 杭州:浙江大学, 2013.

    [42]

    Xu B. Fault characteristics of the Qaidam Basin in early Cenozoic from seismic attributes analysis[D]. Hangzhou:Zheng Jiang University, 2013.

    [43]

    Wu L, Xiao A, Wang L, et al. EW-trending uplifts along the southern side of the central segment of the Altyn Tagh Fault,NW China: Insight into the rising mechanism of the Altyn Mountain during the Cenozoic[J]. Science China Earth Sciences, 2012, 55(6):926-939.

    [44]

    毛黎光, 肖安成, 王亮, 等. 柴达木盆地西北缘始新世晚期古隆起与阿尔金断裂的形成[J]. 岩石学报, 2013, 29(8):2876-2882.

    [45]

    Mao L G, Xiao A C, Wang L, et al. Uplift of NW margin of Qaidam Basin in the Late Eocene:Implications for the initiation of Altyn Fault[J]. Acta Petrologica Sinica, 2013, 29(8):2876-2882.

    [46]

    Qiu N S. Tectono-thermal evolution of the Qaidam Basin,China:Evidence from Ro and apatite fission track data[J]. Petroleum Geoscience, 2002, 8(3):279-285.

    [47]

    罗群, 庞雄奇. 运用断裂控烃理论实现柴达木盆地油气勘探大突破[J]. 石油学报, 2003, 24(2):24-29.

    [48]

    Luo Q, Pang X Q. Application of fault control hydrocarbon theory to realize a great breakthrough of petroleum exploration in Qaidam basin[J]. Acta Petrolei Sinica, 2003, 24(2):24-29.

    [49]

    Pang X Q, Li Y X, Jiang Z X. Key geological controls on migration and accumulation for hydrocarbons derived from mature source rocks in Qaidam Basin[J]. Journal of Petroleum Science and Engineering, 2004, 41(1):79-95.

    [50]

    Zeng L, Tang X, Wang T, et al. The influence of fracture cements in tight Paleogene saline lacustrine carbonate reservoirs,western Qaidam Basin,northwest China[J]. AAPG Bulletin, 2012, 96(11):2003-2017.

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出版历程
收稿日期:  2021-02-23
修回日期:  2021-10-20
刊出日期:  2021-12-15

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