南海北部白云凹陷继承性陆缘背景古潜山成因及类型

刘军; 彭光荣; 张丽丽; 李洪博; 汪旭东; 吴哲; 官伟; 梁超; 黄雷

doi:10.3799/dqkx.2023.187

南海北部白云凹陷继承性陆缘背景古潜山成因及类型

doi: 10.3799/dqkx.2023.187

刘军^{1, 2,},
彭光荣^{1, 2},
张丽丽^{1, 2},
李洪博^{1, 2},
汪旭东^{1, 2},
吴哲^{1, 2},
官伟³,
梁超³,
黄雷^3, , ,

1.
中海石油(中国)有限公司深圳分公司, 广东深圳 518054
2.
中海石油深海开发有限公司, 广东深圳 518000
3.
西北大学含油气盆地研究所, 陕西西安 710069

基金项目:

中国海洋石油有限公司前瞻基础研究项目《南海东部地区前新生界石油地质条件及勘探潜力》 KJQZ-2024-2004

中海石油（中国）有限公司重大项目“南海大中型天然气田形成条件、勘探潜力与突破方向” KJZH-2021-0003

中海石油（中国）有限公司“十四五”科技攻关项目“中国近海新区新领域勘探技术” KJGG2022-0302

国家自然科学基金项目 42272148

详细信息

作者简介:
刘军（1973-），男，教授级高级工程师，主要从事油气勘探相关研究工作. E-mail：liujun1@cnooc.com.cn

通讯作者:
黄雷，ORCID: 0000-0002-7257-2062. E-mail: huanglei@nwu.edu.cn

中图分类号: P618.13
计量
- 文章访问数: 288
- HTML全文浏览量: 117
- PDF下载量: 32
- 被引次数: 0
出版历程
- 收稿日期: 2023-11-15
- 网络出版日期: 2025-02-26
- 刊出日期: 2025-02-25

Genesis and Types of Buried Hills in the Tectonic Setting of the Inheriting Continental Margin in Baiyun Sag, Northern South China Sea

Liu Jun^{1, 2
,},
Peng Guangrong^{1, 2},
Zhang Lili^{1, 2},
Li Hongbo^{1, 2},
Wang Xudong^{1, 2},
Wu Zhe^{1, 2},
Guan Wei³,
Liang Chao³,
Huang Lei^{3
, ,
,}

1.
Shenzhen Branch of CNOOC Ltd., Shenzhen 518054, China
2.
China National Offshore Oil Corporation Deepwater Development Ltd., Shenzhen 518000, China
3.
Institute of Oil and Gas Basin, Northwest University, Xi`an 710069, China

摘要

摘要: 白云凹陷潜山是南海北部珠江口盆地油气勘探向深水深层进军的现实领域之一，目前对潜山成因及分类的研究相对薄弱，制约潜山带油气勘探潜力的评价. 利用大面积三维地震资料，考虑继承性陆缘背景的构造相互作用关系，开展白云凹陷潜山构造解析. 识别出了基底内幕的中生代先存构造，新生代拆离断裂体系和多期次岩浆活动，以及走滑断裂体系. 明确白云凹陷潜山的形成是中生代挤压构造，新生代伸展拆离和岩浆底侵耦合及晚期断裂改造的结果. 基于上述主控因素提出白云凹陷潜山分类方案，该地区潜山划分为中生代构造主控的地貌残丘型，新生代早期构造主控的伸展块断型以及后期改造型共3大类6小类. 其中白云主洼北部的冲断残丘型和白云主洼东部的翘倾断块型以及白云西南部断垒型和走滑块断型潜山具有良好的花岗岩潜山储层发育条件，是寻找潜山圈闭的有利区.
- 南海北部 /
- 白云凹陷 /
- 潜山 /
- 先存构造 /
- 拆离断裂 /
- 岩浆作用 /
- 成因类型 /
- 石油地质
Abstract: The buried hill in the Baiyun Sag is one of the deep-water oils and gas exploration fields in the Pearl River Mouth Basin in the northern South China Sea. However, research on the origin and classification of buried hills is relatively weak, which restricts the evaluation of the oil and gas exploration potential of buried hills. Structural analysis of buried hills in the Baiyun Sag from the perspective of inherited continental margin tectonic background using large-scale 3D seismic data. Mesozoic preexisting structures, Cenozoic detachment fault systems and multiple phases of magmatism, and strike-slip fault systems are identified. The buried hill in the Baiyun Sag is affected by three main controlling factors: pre-existing basement structure, detachment fault and late magmatic transformation. The buried hills in this area can be divided into three types and six subtypes: the geomorphic residual hill dominated by the Mesozoic structure, the extensional fault block dominated by the early Cenozoic structure, and the later modified buried hills. Among them, the thrust residual hill in the northern Baiyun sag, the tilting fault block in the eastern Baiyun sag and the horst and fault blockformed by normal and strike-slip faults of different orientations in the southwestern Baiyun sag have good granite reservoir development conditions, and is the favorable area to search for traps.
- Northern South China Sea /
- Baiyun Sag /
- buried hill /
- pre-existing structure /
- Detachment fault /
- Magmatism /
- Genesis and types of buried hills /
- petroleum geology

HTML全文

图 1 南海北部白云凹陷构造单元和潜山地貌图及地层柱状图

Fig. 1. Structural unit and buried hill topographic map and stratigraphic histogram of the Baiyun Sag, northern South China Sea

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图 2 白云凹陷西南部潜山内幕中生代先存断裂典型剖面（位置见图 1）

Fig. 2. Typical profiles of Mesozoic pre-existing faults in the buried hill sat the southwestern Baiyun Sag (see location in Fig. 1)

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图 3 潜山形成主控因素典型剖面

a. 基底内幕先存断裂（位置见图 5）；b. 拆离断层及伴生岩浆活动及断块旋转（位置见图 7a）；c. 多期次岩浆活动特征（位置见图 1）；d. NW走向走滑断裂花状构造（位置见图 9）

Fig. 3. Typical profiles of the main controlling factors for the formation of buried hills

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图 4 白云凹陷及周缘潜山成因类型划分方案

Fig. 4. Genetic classification scheme of buried hills in the Baiyun Sag

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图 5 白云凹陷北部冲断残丘型潜山剖面（位置见图 1）

Fig. 5. Residual mound buried hill controlled by thrust faults in the northern Baiyun Sag(see location in Fig. 1)

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图 6 白云凹陷西南部逆冲褶皱型潜山剖面（位置见图 1）

Fig. 6. Thrust fold buried hill in the southwestern Baiyun Sag(see location in Fig. 1)

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图 7 白云主洼东低角度块断型潜山剖面（位置见图 1）

Fig. 7. Fault block buried hill controlled by low angle faults in the eastern part of the main Baiyun Sag(see location in Fig. 1)

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图 8 白云主洼东拆离-岩浆底侵型潜山剖面（位置见图 1）

Fig. 8. Buried hill controlled by detachment fault-magmatism in the eastern part of the main Baiyun Sag(see location in Fig. 1)

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图 9 白云凹陷西南部高角度断层块断型潜山剖面（位置见图 1）

Fig. 9. Fault block buried hill controlled by high angle normal faults in the southwestern Baiyun Sag(see location in Fig. 1)

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图 10 白云凹陷西南部断裂差异活动型潜山剖面（位置见图 1）

Fig. 10. Fault differential activity type buried hill in the southwestern Baiyun Sag(see location in Fig. 1)

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图 11 白云主洼东岩浆底辟型潜山剖面（位置见图 1）

Fig. 11. Magmatic diapir buried hill in the eastern part of main Baiyun Sag(see location in Fig. 1)

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图 12 白云主洼断裂与岩浆底辟复合型潜山剖面（位置见图 1）

Fig. 12. Faults and magmatic diapir compound buried hill in the main Baiyun Sag(see location in Fig. 1)

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