珠江口盆地阳江东凹早新生代洼陷结构差异及其控制机制分析

沈梦蓉; 单玄龙; 郝国丽; 刘培; 贾培蒙; 徐川; 张志伟; 汪晓萌

doi:10.3799/dqkx.2022.078

珠江口盆地阳江东凹早新生代洼陷结构差异及其控制机制分析

doi: 10.3799/dqkx.2022.078

1.
吉林大学地球科学学院, 吉林长春 130061
2.
中海石油(中国)有限公司深圳分公司, 广东深圳 518000

基金项目:

中海石油重大科技专项“南海东部油田上产2 000万吨关键技术研究” CN00C-KJ135ZDXM37SZ

国家自然科学基金重大项目 41790453

国家自然科学基金面上项目 41972313

详细信息

作者简介:
沈梦蓉（1997-），女，硕士研究生，主要从事盆地构造和石油地质工作.E-mail：shenmr0523@qq.com

通讯作者:
单玄龙，E-mail: shanxl@jlu.edu.cn

中图分类号: P548
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- 被引次数: 0
出版历程
- 收稿日期: 2023-01-14
- 刊出日期: 2024-10-25

Structural Difference and Control Mechanism of Early Cenozoic Depression in Yangjiang East Sag, Pearl River Mouth Basin

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
Shenzhen Branch, CNOOC China Limited, Shenzhen 518000, China

摘要

摘要: 为探究珠三坳陷阳江东凹洼陷结构差异及其控制机制，利用三维地震数据精细解释了该凹陷主要断裂的发育特征并分析了其活动性，识别并总结了岩浆底辟的分布特征，系统地研究了阳江东凹早新生代不同洼陷的构造差异性.研究表明，阳江东凹特殊的构造位置影响了凹陷的形成，构造转换带控制了研究区各洼陷差异发育.西部阳江24洼呈北断南超的简单半地堑结构，中部和东部恩平19、20、21洼呈南北双断的复式半地堑结构.区域应力场下洼陷伸展方式的不同导致裂陷初始期的岩石圈地壳变形存在差异，同裂陷期岩浆运移至压力较小的转换带下方并聚集形成岩浆房，基底深大断裂沟通地壳深部，控制了岩浆上涌和侵位.岩浆的热作用使得地壳脆性变形转变为韧性变形，地壳的快速减薄及NE、NEE向先存断裂在深大断裂转折处发育的构造转换带控制了盆地构造样式.因此靠近阳江-一统暗沙断裂带的洼陷发育斜滑断裂并呈复式半地堑结构.上述分析为研究区烃源岩预测及勘探提供了理论依据.
- 珠江口盆地 /
- 阳江东凹 /
- 转换带 /
- 阳江-一统暗沙断裂带 /
- 岩浆活动 /
- 动力学 /
- 石油地质学
Abstract: In order to explore the structural difference and control mechanism of Yangjiang east sag in Zhusan depression, the development characteristics of main faults in the sag are finely explained and their activity is analyzed by using three-dimensional seismic data, the distribution characteristics of magmatic diapir are identified and summarized, and the structural differences of different depressions in Yangjiang east sag in Early Cenozoic are systematically studied. The study shows that the special structural position of Yangjiang east sag influences the formation of the sag, and the structural transformation zone controls the differential development of each sag in the study area. Yangjiang No.24 depression in the west is a simple half graben structure with north fault and south overlap, while Enping No.19, No.20 and No.21 depressions in the middle and east is a compound half graben structure with north-south double faults. The deformation of lithospheric crust in the initial stage of rifting is different due to the different extension modes of subsag under the regional stress field. During the same rifting stage, the magma migrated to the lower pressure transition zone and accumulated to form magma chamber. The deep faults in the basement communicated with the deep crust and controlled the magma upwelling and emplacement. The thermal action of magma makes the crustal brittle deformation change into ductile deformation, so the sag near the Yangjiang-Yitong'ansha blind fault zone develops oblique slip fault and presents a compound half graben structure. The above analysis provides a theoretical basis for the prediction and exploration of source rocks in the study area.
- Pearl River Mouth Basin /
- Yangjiang east sag /
- transfer zone /
- Yangjiang-Yitong'ansha blind fault zone /
- magmatism /
- dynamic mechanism /
- petroleum geology

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图 1 阳江东凹构造纲要

a.珠江口盆地区域位置；b.阳江凹陷位置；c.阳江东凹构造单元划分. 据田立新等（2020）；陈长民等（2003）修改

Fig. 1. Outline drawing of Yangjiang east sag structure

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图 2 阳江东凹构造-地层格架

Fig. 2. Structural stratigraphic framework of Yangjiang east sag

下载: 全尺寸图片幻灯片

图 3 阳江东凹典型洼陷结构地震剖面(位置见图 5)

Fig. 3. Seismic profile of typical depression structure in Yangjiang east sag

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图 4 阳江东凹剖面结构变化

Fig. 4. Structural change of Yangjiang east sag section

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图 5 阳江东凹文昌组顶面主要断层及岩浆底辟构造平面展布

Fig. 5. Plane distribution of main faults and magmatic diapir structures on the top of Wenchang Formation in Yangjiang east sag

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图 6 阳江东凹各时期控洼断层沿走向延伸长度-断距柱状图

Fig. 6. Histograms of the extended length of the depression-controlling faults along the strike-distance in each period in the Yangjiang east sag

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图 7 岩浆底辟构造类型模式

a.隐伏底辟-沉积后期；b.刺穿底辟-同沉积期；c.隐伏底辟-同沉积期；d.刺穿底辟-沉积后期

Fig. 7. Model map of magmatic diapir structure type

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图 8 阳江东凹各洼陷典型岩浆底辟解释图(位置见图 3)

Fig. 8. Interpretation of typical magmatic diapir in each sag of Yangjiang east sag

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图 9 转换带模式

据Morley et al.（1990）修改

Fig. 9. Transfer zone model diagram

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图 10 斜向伸展下岩浆侵位模式

据Corti et al.（2003）修改

Fig. 10. Emplacement model of magma under oblique extension

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表 1 阳江东凹裂陷期洼陷结构样式特征统计

Table 1. Structural style characteristics of Wenchang Formation in Yangjiang east sag

洼陷名称	最大残余厚度（m）	控洼断裂	结构样式	洼陷形态
阳江24洼	2 000	F1	半地堑	北断南超
恩平19洼	800	F3	复式半地堑	早期南断北超，晚期双断
恩平20洼	1 300	F4	复式半地堑	北断南超
恩平21洼	1 700	F5、F6	复式半地堑、半地堑	南断北超

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