任建业^1,,
庞雄²,
于鹏³,
雷超¹,
罗盼¹
1. 中国地质大学海洋学院, 武汉 430074
2. 中海石油(中国)有限公司深圳分公司, 广东深圳 518054
3. 同济大学 海洋与地球科学学院, 上海 200092

基金项目: 国家自然科学基金重点项目（41830537）、国家海洋局"全球变化与海气相互作用"专项（GASI-GEOGE-02）、国家自然科学基金"南海计划集成项目"（91528301）和国家重大科技专项（2016ZX005008，2016ZX05026）资助


详细信息

作者简介: 任建业, 男, 1963年生, 教授, 长期从事沉积盆地分析方面的教学和科研工作.E-mail:jyren@cug.edu.cn

中图分类号: P631;P738

收稿日期:2017-09-04
修回日期:2018-07-07
上线日期:2018-12-05

Characteristics and formation mechanism of deepwater and ultra-deepwater basins in the northern continental margin of the South China Sea

REN JianYe^1,,
PANG Xiong²,
YU Peng³,
LEI Chao¹,
LUO Pan¹
1. College of Marine Science and Technology, China University of Geosciences, Wuhan 430074, China
2. China National Offshore Oil CorporationLimited, Guangdong Shenzhen 518054, China
3. College of Marine and Earth Science, Tongji University, Shanghai 200092, China


MSC: P631;P738

--> Received Date: 04 September 2017
Revised Date: 07 July 2018
Available Online: 05 December 2018


摘要
摘要:本文以海洋地质调查和油气勘探开发中积累的地质和地球物理资料的解释和分析为基础，描述和划分了南海北部被动陆缘地壳岩石圈结构构造单元，由陆向海划分出近端带、细颈化带、远端带和洋陆转换带（OCT，含边缘高地）四个构造单元.从细颈化带到OCT基本处于现今陆架坡折带之外的深水-超深水区的范围，以强烈的地壳薄化和发育大型拆离断层控制的拆离盆地为特征.这些深水-超深水盆地的同裂陷阶段均经历了早期均一断陷、中晚期拆离式断陷的演化过程，受控于南海北部大型拆离断层作用及其所导致的岩石圈临界破裂过程.新的深水-超深水盆地形成机理的认识为南海北部陆缘岩石圈的非瞬时伸展破裂过程的分析提供了新的视角，同时，陆缘深水-超深水盆地具有独特的构造-沉积体系配置和构造-热演化过程，将为科学评价南海北部陆缘深水-超深水盆地油气勘探潜力提供新的思路.
关键词: 南海北部陆缘/
深水-超深水盆地/
拆离断层/
非瞬时伸展破裂模式

Abstract:This work is based on the interpretation and analysis geological and geophysical data collected by marine geological investigations and petroleum exploration and production. The purpose is to delineate the architectural elements of the northern continental margin in the South China Sea. From land to sea, this region can be divided into four first-order tectonic units, i.e. the proximal, necking, distal, and the Ocean-Continent Transition (OCT) (including Outer High) zones. The region from the necking to the OCT is largely located in the deepwater and ultra-deepwater area, almost in the southern present-day continental shelf break zone. This region is characterized by the hyper-extended continental crust where a series of large-scale detachment fault systems controlling the supra-detachment rift basin. At the syn-rifted period, the deepwater and ultra-deepwater basins all experienced initial uniform rifting and subsequently detachment rifting, which was related to the detachment faulting and final continental breakup in the northern South China Sea. This new understanding on the formation mechanism for the deepwater and ultra-deepwater basins provides new insights on the non-instantaneous continental extension in the northern South China Sea. In addition, these deepwater and ultra-deepwater basins show a typical tectono-sedimentary configuration and tectono-thermal evolution, which will provide new ideas for scientifically evaluating the potential petroleum exploration in deep/ultra-deep water basins of the northern continental margin of the South China Sea.
Key words:Northern South China Sea/
Deepwater and ultra-deepwater basin/
Detachment fault/
Non-instantaneous extension and breakup model



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