冯旭亮^1,3,,
张功成^2,,,
王万银¹,
赵志刚²,
邱之云¹,
谢晓军²,
纪晓琳¹,
鲁宝亮¹,
宋双²
1. 长安大学重磁方法技术研究所, 长安大学地质工程与测绘学院, 长安大学西部矿产资源与地质工程教育部重点实验室, 西安 710054
2. 中海油研究总院, 北京 100027
3. 西安石油大学地球科学与工程学院, 西安 710065

基金项目: 国家科技重大专项"海洋深水区油气勘探关键技术"（2008ZX05025），中海油研究总院科技项目"重磁震联合研究南海新生代盆地分布与构造区划"，中央高校基本科研业务费专项资金（310826163301）联合资助


详细信息

作者简介: 冯旭亮, 男, 1989年生, 博士, 2016年毕业于长安大学, 现为西安石油大学讲师, 主要从事重、磁勘探方法理论与应用研究及综合地球物理勘探研究及教学工作.E-mail:fxlchd@163.com

通讯作者: 张功成, 男, 1966年生, 博士, 教授级高级工程师, 主要从事石油与天然气地质学研究. E-mail:zhanggch@cnooc.com.cn

中图分类号: P631

收稿日期:2017-09-04
修回日期:2018-09-11
上线日期:2018-10-05

An integrated study on distribution of Cenozoic basins in the South China Sea based on gravity, magnetic and seismic data

FENG XuLiang^1,3,,
ZHANG GongCheng^2,,,
WANG WanYin¹,
ZHAO ZhiGang²,
QIU ZhiYun¹,
XIE XiaoJun²,
JI XiaoLin¹,
LU BaoLiang¹,
SONG Shuang²
1. Institute of Gravity and Magnetic Technology, College of Geology Engineering and Geomatics, Key Laboratory of Western China's Mineral Resources and Geological Engineering, Ministry of Education, Chang'an University, Xi'an 710054, China
2. CNOOC Research Institute, Beijing 100027, China
3. School of Earth Sciences and Engineering, Xi'an Shiyou University, Xi'an 710065, China


More Information

Corresponding author: ZHANG GongCheng,E-mail:zhanggch@cnooc.com.cn

MSC: P631

--> Received Date: 04 September 2017
Revised Date: 11 September 2018
Available Online: 05 October 2018


摘要
摘要:作为西太平洋最大的边缘海，南海分布有30多个新生代沉积盆地，其蕴含着丰富的油气资源.但由于资料的限制，南海存在不同区域盆地研究程度不同，不同区域盆地面积差别较大，部分盆地只是坳陷而没有达到盆地的级别以及盆地外围可能存在凹陷等问题.南海新生代盆地分布问题制约了其油气分布规律、储量等基础地质问题的研究.本文以地震剖面数据为约束，以重力资料为主、辅以磁力资料，研究了南海新生代盆地分布及构造区划.通过提取新生代盆地及其构造单元引起的重力异常，结合地震剖面等资料反演了新生界底界面深度及新生界厚度.在充分调研已有盆地和构造单元划分方案的基础上，根据南海的地质及地球物理特征，确定了盆地及构造单元划分标准.以新生界厚度为基础并结合重、磁、震、地质等资料，进行地质-重磁震联合解释，将南海原有的36个盆地重新划分为24个盆地，盆地总面积扩大了约15万km².研究表明，南海新生代盆地沉积层厚度在1.5~16 km之间，有6个北东东/北东向沉积坳陷带、2个近南北向沉积坳陷带以及1个三角沉积坳陷区；盆地展布方向主要为北东和北东东向，其次为北西和近南北向，呈现"南三北三"的分布特征.
关键词: 南海/
新生代沉积盆地/
重磁震联合解释/
新生界厚度

Abstract:The South China Sea (SCS), as the largest marginal sea in the western Pacific Ocean, hosts more than 30 Cenozoic sedimentary basins that contain abundant oil and gas. Due to the limit of survey data available, some of these basins lack exhaustive studies or have controversial issues, especially in the central and southern regions. For example, different boundaries of basins in the central and southern SCS have been delineated. The relationship between the basins remain unclear and some basins (e.g. Nanweidong basin and Jiuzhang basin) may not attain the level of a true basin, instead merely a depression. In addition, some sags may exist on the periphery of some basins. To address these problems, we have studied the distribution of the Cenozoic basins in the SCS based on gravity, magnetic seismic data in an integrated way.
We collected the latest satellite altimetry gravity and magnetic ΔT anomalies and analyzed the physical properties of the strata and rocks in the SCS. Then we obtained the Bouguer gravity anomalies by removing the effect caused by seawater and computed the magnetic anomalies reduced to the pole using a varying inclination method. Based on the analysis of the characteristics of the gravity field, we extracted the gravity anomalies of the Cenozoic by using the minimum curvature technique for potential field data separation and inverted the thickness of Cenozoic in the study area under the constraint of seismic profiles.
We established the criteria to divide basins and other tectonic units on the basis of the thickness of Cenozoic and the relative relief of the basement assisted with the characteristics of the gravity and magnetic fields and trend lines of the faults combining other geologic data. Then we re-divided the original 36 Cenozoic basins into 24 sedimentary ones and defined their internal tectonic units. The total area of the newly divided basins has increased by about 150 thousand square kilometers. The thickness of the sedimentary layer of Cenozoic basins in the SCS is between 1.5 km and 16 km, which is rather changeable. These basins are divided into six NE or NEE trending sedimentary depression zones, two nearly NS trending sedimentary depression zones and one triangular sedimentary area. The directions of the basin distribution are mainly NE and NEE, followed by NW and nearly NS. Under the control of the major faults, these structures show a 'south three and north three' pattern.
Key words:The South China Sea/
Cenozoic sedimentary basins/
Joint interpretation of gravity magnetic and seismic data/
Cenozoic sedimentary thickness



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