石油勘探与开发 >

2020 , Vol. 47 >Issue 3: 447 - 461

DOI: https://doi.org/10.11698/PED.2020.03.02

油气勘探

珠江口盆地惠州运动及其意义

  • 施和生 ,
  • 杜家元 ,
  • 梅廉夫 ,
  • 张向涛 ,
  • 郝世豪 ,
  • 刘培 ,
  • 邓棚 ,
  • 张琴
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  • 1. 中海石油（中国）有限公司勘探部,北京100010;
    2. 中海石油（中国）有限公司深圳分公司,广东深圳518000;
    3. 中国地质大学（武汉）构造与油气资源教育部重点实验室,武汉430074
施和生（1962-）,男,江苏启东人,博士,中国海洋石油总公司教授级高级工程师,主要从事石油地质及油气勘探综合研究与管理工作。地址：北京市东城区朝阳门北大街25号,中国海洋石油集团有限公司,邮政编码：100010。E-mail: shihsh@cnooc.com.cn

收稿日期: 2019-07-05

  网络出版日期: 2020-05-19

基金资助

国家科技重大专项（2016ZX05026;2016ZX05024-004;2016ZX05026-003-001）

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Huizhou Movement and its significance in Pearl River Mouth Basin, China

  • SHI Hesheng ,
  • DU Jiayuan ,
  • MEI Lianfu ,
  • ZHANG Xiangtao ,
  • HAO Shihao ,
  • LIU Pei ,
  • DENG Peng ,
  • ZHANG Qin
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  • 1. Exploration Department of CNOOC Ltd., Beijing 100010, China;
    2. Shenzhen Branch of CNOOC Ltd., Shenzhen 518000, China;
    3. Key Laboratory of Tectonics and Petroleum Resources, Ministry of Education, China University of Geosciences, Wuhan 430074, China

Received date: 2019-07-05

  Online published: 2020-05-19

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摘要

惠州运动指发生在珠江口盆地中始新世早、晚文昌期（距今43 Ma）之间的构造运动。基于地震、测井、地质、钻井等资料,综合运用断裂特征分析、剥蚀厚度恢复、岩浆作用统计、区域构造动力学比对等方法,揭示惠州运动的特征、属性及动力学机制。惠州运动主要表现为裂陷作用的南北转变和沿断裂走向的迁移、基底隆升、岩浆底辟以及地层剥蚀等。研究认为惠州运动是珠江口盆地周缘板块相互作用和岩石圈减薄过程的综合反映,特别是与岩石圈由初始张裂到快速减薄的变化、以及印度—欧亚大陆开始硬碰撞、太平洋板块俯冲方向的变化有紧密的动力学成因联系。惠州运动对珠江口盆地古近系富生烃凹陷和烃源岩发育、沉积体系和深部优质储集层形成、油气成藏等具有重要的影响。图15表2参42

关键词： 惠州运动; 油气成藏; 始新世; 古近系; 珠江口盆地

本文引用格式

施和生 , 杜家元 , 梅廉夫 , 张向涛 , 郝世豪 , 刘培 , 邓棚 , 张琴 . 珠江口盆地惠州运动及其意义[J]. 石油勘探与开发, 2020 , 47(3) : 447 -461 . DOI: 10.11698/PED.2020.03.02

Abstract

The Huizhou Movement refers to the Middle Eocene tectonic transition from the early to late Wenchang Rift stages (about 43 Ma ago) in the Pearl River Mouth Basin. Based on seismic reflection, drilling, logging and geological data, the fault characteristic analysis, denudation thickness recovery, magmatism statistics, regional tectonic dynamics comparison and other methods are used to reveal the characteristics, properties and dynamic mechanism of the Huizhou Movement. The Huizhou Movement mainly shows the North-South transition of rifting and the migration along the faults, basement uplift, magmatic diapir and stratigraphic denudation. It is believed that the Huizhou Movement is a comprehensive reflection of plate interaction and lithospheric thinning process in the Pearl River Mouth Basin, which is closely related to the transition of lithosphere from initial rifting to rapid thinning, the India-Eurasia hard collision and the change of subduction direction of the Pacific plate. The Huizhou Movement has important influence and restriction on Paleogene hydrocarbon-generating sags and the development of hydrocarbon source rocks, sedimentary system and deep high-quality reservoir, hydrocarbon migration and accumulation in the Pearl River Mouth Basin.

Key words： Huizhou Movement; hydrocarbon accumulation; Eocene; Paleocene; Pearl River Mouth Basin

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