塔里木盆地顺北5号走滑断裂带分层分段特征及构造演化

doi:10.7657/XJPG20230105

新疆石油地质 ›› 2023, Vol. 44 ›› Issue (1): 33-42.doi: 10.7657/XJPG20230105

塔里木盆地顺北5号走滑断裂带分层分段特征及构造演化

陈平^1a^,^1b(), 能源^1b^,²(), 吴鲜³, 黄诚³, 王来源³, 郭曼²

1a.地球科学学院,中国石油大学（北京）, 北京 102249
1b.油气资源与探测国家重点实验室,中国石油大学（北京）, 北京 102249
2.中国石油大学（北京）克拉玛依校区石油学院,新疆克拉玛依 834000
3.中国石化西北油田分公司,乌鲁木齐 830011

收稿日期:2021-12-16 修回日期:2022-05-12 出版日期:2023-02-01 发布日期:2023-02-03
通讯作者: 能源（1982-），男，黑龙江大庆人，教授，博士，构造地质学及油区构造解析，（Tel）0990-6633553（E-mail）nengyuan@foxmail.com
作者简介:陈平（1995-），男，重庆万州人，硕士，地质学，（Tel）17610770520（E-mail）243801601@qq.com
基金资助:
新疆维吾尔自治区自然科学基金(2021D01A199);自治区高校科研计划项目(XJEDU2019Y072)

Stratification and Segmentation Characteristics and Tectonic Evolution of Shunbei No.5 Strike-Slip Fault Zone in Tarim Basin

CHEN Ping^1a^,^1b(), NENG Yuan^1b^,²(), WU Xian³, HUANG Cheng³, WANG Laiyuan³, GUO Man²

1a. School of Earth Sciences, China University of Petroleum, Beijing 102249, China
1b. State Key Laboratory of Oil and Gas Resources and Exploration, China University of Petroleum, Beijing 102249,China
2. Petroleum College,Karamay Campus,China University of Petroleum (Beijing),Karamay,Xinjiang 834000,China
3. Northwest Oilfield Company, Sinopec, Urumqi, Xinjiang 830011, China

Received:2021-12-16 Revised:2022-05-12 Online:2023-02-01 Published:2023-02-03

摘要/Abstract

摘要：

塔里木盆地超深层断溶体油气藏主要沿走滑断裂带分布，远离断裂带地区油气勘探效果差，即走滑断裂带的活动规模控制了油气藏的规模。顺北5号走滑断裂带为超大型走滑断裂带，具有埋藏深，内部结构复杂，分层分段性极强的特点。通过高品质三维地震资料，对顺北5号走滑断裂带进行系统的几何学、运动学和动力学研究，提出以下认识：顺北5号走滑断裂带具有极强的分层性，可划分为5个构造层；该断裂带分段活动特征明显，南段和北段具不同的运动学特征，南段经历了5期演化，北段经历了4期演化。

关键词: 塔里木盆地, 顺北5号走滑断裂带, 超深层, 断溶体油气藏, 构造层, 分段活动, 多层结构, 多期运动

Abstract:

The ultra-deep fault-karst reservoirs in the Tarim basin are mainly distributed along strike-slip fault zones，and the oil and gas exploration effects are poor in the areas far away from fault zones，that is，the activity scale of strike-slip fault zones control the scale of hydrocarbon accumulation. The Shunbei No.5 strike-slip fault zone is a super-large strike-slip fault zone，which is characterized by deep burial，complex internal structure，and evident stratification and segmentation. Based on high-quality 3D seismic data，the geometry，kinematics and dynamics of the Shunbei No.5 strike-slip fault zone were systematically analyzed. It is recognized that the Shunbei No.5 strike-slip fault zone is evidently layered (including 5 structural layers)，and also segmented，with the southern and northern segments having different kinematic characteristics. The southern segment has experienced 5 stages of evolution，and the northern segment has experienced 4 stages of evolution.

Key words: Tarim basin, Shunbei No.5 strike-slip fault zone, ultra-deep layer, fault-karst reservoir, structural layer, segmented activity, multi-layered structure, multi-stage movement

中图分类号:

TE121

陈平, 能源, 吴鲜, 黄诚, 王来源, 郭曼. 塔里木盆地顺北5号走滑断裂带分层分段特征及构造演化[J]. 新疆石油地质, 2023, 44(1): 33-42.

CHEN Ping, NENG Yuan, WU Xian, HUANG Cheng, WANG Laiyuan, GUO Man. Stratification and Segmentation Characteristics and Tectonic Evolution of Shunbei No.5 Strike-Slip Fault Zone in Tarim Basin[J]. Xinjiang Petroleum Geology, 2023, 44(1): 33-42.

图/表 10

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塔里木盆地顺北5号走滑断裂带分层分段特征及构造演化

Stratification and Segmentation Characteristics and Tectonic Evolution of Shunbei No.5 Strike-Slip Fault Zone in Tarim Basin

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