塔里木盆地北缘沙雅隆起两阶段走滑变形的证据

何光玉; 顾忆; 赵永强; 姚泽伟; 郑晓丽; 肖思东; 黄继文; 贾存善; 周雨双

doi:10.11781/sysydz202002172

塔里木盆地北缘沙雅隆起两阶段走滑变形的证据

doi: 10.11781/sysydz202002172

何光玉^1,,
顾忆²,
赵永强²,
姚泽伟^{1, 3},
郑晓丽⁴,
肖思东^{1, 5},
黄继文²,
贾存善²,
周雨双²

1.
浙江大学地球科学学院, 杭州 310027
2.
中国石化石油勘探开发研究院无锡石油地质研究所, 江苏无锡 214126
3.
浙江大学海洋学院, 浙江舟山 316021
4.
东方地球物理公司, 新疆库尔勒 841000
5.
浙江国高能源科技有限公司, 杭州 310023

基金项目:

国家“十三五”科技攻关项目 2017ZX05005002-002

详细信息

作者简介:
何光玉(1968-), 男, 博士, 副教授, 从事构造地质、石油地质与海洋地质教学和研究。E-mail: hegy@zju.edu.cn

中图分类号: TE121.1
计量
- 文章访问数: 753
- HTML全文浏览量: 365
- PDF下载量: 140
- 被引次数: 0
出版历程
- 收稿日期: 2019-12-07
- 修回日期: 2020-02-07
- 刊出日期: 2020-03-28

Evidence of two-stage strike-slip structural deformation of Shaya Uplift, northern Tarim Basin

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

摘要

摘要: 沙雅隆起（塔北隆起）是塔里木盆地北缘极为重要的近东西向构造带。前人研究认为，沙雅隆起以逆冲变形为主，但是，这一认识既与地震剖面上的花状构造样式相矛盾，又与平面图上断层呈扫帚状和拖尾状分布的特征相矛盾。该文基于高分辨率的三维地震剖面，提出塔里木盆地北缘沙雅隆起经历了2个阶段的走滑构造变形：第一阶段为加里东晚期—印支期的压扭构造变形，形成了深部构造层中的大型正花状构造，同时地层被大幅抬升并遭受剥蚀；第二阶段为喜马拉雅期的负反转—张扭构造变形，形成了浅部构造层中的负花状构造。这一认识表明，塔里木盆地北缘可能并非统一的构造—沉积环境，沙雅走滑构造带为一重要的构造—沉积分隔带，而加里东晚期与喜马拉雅早期是塔里木盆地北缘非常重要的2个构造变革期。
- 走滑构造 /
- 花状构造 /
- 构造变革 /
- 沙雅隆起 /
- 塔里木盆地
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.
- strike-slip /
- flower structure /
- structural transform /
- Shaya Uplift /
- Tarim Basin

HTML全文

图 1 塔里木盆地沙雅隆起构造位置

F1.轮台断裂；F2.亚南断裂；F3.轮南断裂；F4.喀拉玉尔滚断裂；F5.羊塔克断裂；F6.英买7断裂

Figure 1. Tectonic location of Shaya Uplift, Tarim Basin

下载: 全尺寸图片幻灯片

图 2 塔里木盆地沙雅隆起轮台地区A-A’测线地震剖面

剖面位置见图 1。
F₁.轮台南断裂；F₂.轮台断裂；F₃.雅克拉断裂；F₄.亚南断裂；F₅.库南断裂

Figure 2. Seismic profile A-A' of Luntai area, Shaya Uplift, Tarim Basin

下载: 全尺寸图片幻灯片

图 3 塔里木盆地沙雅隆起库南地区B-B’测线地震剖面

剖面位置见图 1。
F₁.轮台南断裂；F₂.轮台断裂；F₃.轮台北①号断裂；F₄.轮台北②号断裂；F₅.雅克拉断裂；F₆.亚南断裂；F₇.库南断裂

Figure 3. Seismic profile B-B' of Kunan area, Shaya Uplift, Tarim Basin

下载: 全尺寸图片幻灯片

图 4 塔里木盆地沙雅隆起雅克拉断凸带白垩系底面断层分布

平面图位置见图 1。

Figure 4. Fault distribution of Cretaceous in Yakela Fault Uplift, Shaya Uplift, Tarim Basin

下载: 全尺寸图片幻灯片

参考文献(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.