准噶尔盆地周缘断裂属性与演化

doi:10.7623/syxb202109004

石油学报 ›› 2021, Vol. 42 ›› Issue (9): 1163-1173.DOI: 10.7623/syxb202109004

准噶尔盆地周缘断裂属性与演化

朱明, 袁波, 梁则亮, 杨迪生, 唐雪颖

中国石油新疆油田公司勘探开发研究院新疆克拉玛依 834000

收稿日期:2020-09-17 修回日期:2021-03-31 出版日期:2021-09-25 发布日期:2021-10-12
通讯作者: 朱明,男,1975年10月生,1997年获石油大学学士学位,2009年获西南石油大学硕士学位,现为中国石油新疆油田公司勘探开发研究院副院长、高级工程师,主要从事油气勘探综合研究与管理研究。
作者简介:朱明,男,1975年10月生,1997年获石油大学学士学位,2009年获西南石油大学硕士学位,现为中国石油新疆油田公司勘探开发研究院副院长、高级工程师,主要从事油气勘探综合研究与管理研究。Email:zhm@petrochina.com.cn
基金资助:
国家科技重大专项（2016ZX05003-005，2016ZX05047-001-004）和中国石油天然气集团公司科技重大专项（2017E-0403）资助。

Fault properties and evolution in the periphery of Junggar Basin

Zhu Ming, Yuan Bo, Liang Zeliang, Yang Disheng, Tang Xueying

Research Institute of Petroleum Exploration and Development, PetroChina Xinjiang Oilfield Company, Xinjiang Kalamay 834000, China

Received:2020-09-17 Revised:2021-03-31 Online:2021-09-25 Published:2021-10-12

摘要/Abstract

摘要： 准噶尔盆地周缘发育晚古生代、中生代和新生代3期变形。晚古生代，天山—阿尔泰山—扎伊尔山—哈拉阿拉特山隆升，形成盆-山构造雏型；晚二叠世—侏罗纪，盆地周缘发育走滑断层，如：西北缘的乌夏断层、克百断层、红车断层等走滑断层，东北缘的红岩断层、克拉美丽断层、白家海断层等走滑断层，南缘的高泉断层、艾卡断层、南安集海断层、后峡拉分盆地等走滑构造。无论是从构造变形的运动学机制分析还是考虑构造变形时间的一致性，晚二叠世—侏罗纪准噶尔盆地周缘均发育右旋走滑断层。新生代天山再次隆升，南缘发育逆冲断层，与中生代构造叠加，形成"二期构造、深浅叠置"的构造格局。准噶尔盆地西北缘和东北缘的新生代变形微弱，保留了中生代走滑构造，发育与走滑构造有关的油气藏。准噶尔盆地南缘高探1井、呼探1井的勘探成果证实了走滑断层与逆冲构造叠加部位是有利的勘探目标。厘定准噶尔盆地的断裂特征和变形机制对地震解释和油气勘探具有重要意义。

关键词: 准噶尔盆地, 走滑断层, 逆冲断层, 中生代, 新生代

Abstract: There are three periods of deformation occurred in the Late Paleozoic, Mesozoic and Cenozoic in the periphery of Junggar Basin. In Late Paleozoic, the Tianshan Mountains, Altai Mountains, Zaire Mountain and Halaalate Mountains uplifted and formed the basin-mountain tectonic framework. From Late Permian to Jurassic, strike-slip faults developed around the basin, such as the Wuxia fault, Kebai fault and Hongche fault in the northwest margin, the Hongyan fault, Karamaili fault and Baijiahai fault in the northeast margin, as well as the Gaoquan fault, Aika fault, South Anjihai fault and Houxia pull-apart basin in the southern margin. No matter from the perspective of the kinematic mechanism of structural deformation or the consistency in structural deformation time, dextral strike-slip faults developed in the periphery of Junggar Basin from Late Permian to Jurassic. The Tianshan Mountains uplifted again in the Cenozoic, and thrust faults developed in the southern margin of Junggar Basin, which superimposed with Mesozoic structures, forming a tectonic framework with two-stage deformation and superimposed deep and shallow structures. The Cenozoic deformation in the northwest and northeast margins of Junggar Basin was weak, Mesozoic strike-slip structures were preserved, and oil and gas reservoirs related to strike-slip structures were developed. The exploration results of Well Gaotan1 and Well Hutan1 prove that the superimposed region of strike-slip fault and thrust structure is a favorable exploration target in the southern margin of Junggar Basin. Determination of the fault characteristics and deformation mechanism of Junggar Basin is crucial to seismic interpretation and oil and gas exploration.

Key words: Junggar Basin, strike-slip fault, thrust fault, Mesozoic, Cenozoic

中图分类号:

TE121.2

朱明, 袁波, 梁则亮, 杨迪生, 唐雪颖. 准噶尔盆地周缘断裂属性与演化[J]. 石油学报, 2021, 42(9): 1163-1173.

Zhu Ming, Yuan Bo, Liang Zeliang, Yang Disheng, Tang Xueying. Fault properties and evolution in the periphery of Junggar Basin[J]. Acta Petrolei Sinica, 2021, 42(9): 1163-1173.

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准噶尔盆地周缘断裂属性与演化

Fault properties and evolution in the periphery of Junggar Basin

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