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东海盆地椒江凹陷裂后期岩浆作用类型、活动期次及油气地质意义

何新建 覃军 叶青 张朋 梅廉夫 冯桢鸣

海相油气地质2024,Vol.29Issue(4):423-436,14.
海相油气地质2024,Vol.29Issue(4):423-436,14.DOI:10.3969/j.issn.1672-9854.2024.04.008

东海盆地椒江凹陷裂后期岩浆作用类型、活动期次及油气地质意义

Types,activity periods,and petroleum geological significance of post-rift magmatism in Jiaojiang Sag,East China Sea Basin

何新建 1覃军 1叶青 2张朋 3梅廉夫 2冯桢鸣1

作者信息

  • 1. 中海石油(中国)有限公司上海分公司
  • 2. 中国地质大学(武汉)构造与油气资源教育部重点实验室
  • 3. 中国地质大学(北京)海洋学院||中国地质大学(北京)极地地质与海洋矿产教育部重点实验室
  • 折叠

摘要

Abstract

Post-rift magma is widely distributed in Jiaojiang Sag,East China Sea Basin.However,the type,spatial distribution and formation period of magmatism have not been systematically studied,which seriously limits the oil and gas exploration and deployment in the basin.Based on the newly acquired high-precision 3D seismic data,drilling data,this paper identifies and finely describes the magma in the post-rift period,and determines the development regulation of magmatism and the control effects on oil and gas accumulation in Jiaojiang Sag.The results show that the volcanic rocks are mainly distributed in the central and eastern parts of Jiaojiang Sag,with overflow facies as the main type.They are developed along the T20 interface and up and down,but more developed along the T20 interface.There are three types of occurrences of magma intrusion,including saucer,sill,and dike,with saucer being the main occurrence.The emplacement of magma intrusions in the Jiaojiang Sag mainly include three stages:before the Wenzhou stage(>43 Ma),during the Pinghu-Huagang stage(43-23.3 Ma),during and after Longjing stage(<23.3 Ma),and the Pinghu-Huagang stage is the most important period for magma intrusion.The distribution of magma intrusion channels in the study area are related to the northwest striking basement hidden faults,but separated from the Cenozoic faults and have no symbiotic relationship between them.It is traditionally suggested that the magmatism in the post-rift stage may cause damage or alteration to early oil and gas reservoirs,therefore,when selecting potential targets,efforts should be made to avoid the influence of magmatic activity as much as possible.On the other hand,magma intrusion has formed a large number of forced anticlines,and their formation time is later than the peak period of oil and gas generation,which belongs to a good potential trap type.Therefore,these forced anticlines in the magma-rich activity area within Jiaojiang Sag are still worth exploring.

关键词

火山活动/岩浆侵入/伴生构造/裂后期/椒江凹陷/东海盆地

Key words

volcanic activity/magma intrusion/associated structures/post-rift stage/Jiaojiang Sag/East China Sea Basin

分类

能源科技

引用本文复制引用

何新建,覃军,叶青,张朋,梅廉夫,冯桢鸣..东海盆地椒江凹陷裂后期岩浆作用类型、活动期次及油气地质意义[J].海相油气地质,2024,29(4):423-436,14.

基金项目

本文受中海油"十四五"重大科技项目子课题"丽水—椒江凹陷早降晚抬背景下烃源岩与运汇单元研究"(编号:KJGG2022-0301)资助 (编号:KJGG2022-0301)

海相油气地质

OA北大核心CSTPCD

1672-9854

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