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[1]宛良伟 吴 奎 王 伟 加东辉 王启明.辽中南洼旅大16-3地区走滑型源-汇体系发育特征及沉积响应[J].中国海上油气,2019,31(06):34-43.[doi:10.11935/j.issn.1673-1506.2019.06.004]
 WAN Liangwei WU Kui WANG Wei JIA Donghui WANG Qiming.Developmental characteristics and sedimentary response of the strike-slip source-sink system in LD16-3 area of the southern Liaozhong sag[J].China Offshore Oil and Gas,2019,31(06):34-43.[doi:10.11935/j.issn.1673-1506.2019.06.004]
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辽中南洼旅大16-3地区走滑型源-汇体系发育特征及沉积响应()

《中国海上油气》[ISSN:1673-1506/CN:11-5339/TE]

卷:
第31卷
期数:
2019年06期
页码:
34-43
栏目:
渤海海域油气勘探开发成果专辑
出版日期:
2019-11-21

文章信息/Info

Title:
Developmental characteristics and sedimentary response of the strike-slip source-sink system in LD16-3 area of the southern Liaozhong sag
文章编号:
1673-1506(2019)06-0034-10
作者:
宛良伟 吴 奎 王 伟 加东辉 王启明
(中海石油(中国)有限公司天津分公司 天津 300459)
Author(s):
WAN Liangwei WU Kui WANG Wei JIA Donghui WANG Qiming
(CNOOC China Limited, Tianjin Branch, Tianjin 300459, China)
关键词:
辽中南洼 旅大16-3地区 走滑型源-汇体系 发育特征 沉积响应
Keywords:
southern Liaozhong sag LD16-3 area strike-slip source-sink system developmental characteristics sedimentary response
分类号:
TE122.2
DOI:
10.11935/j.issn.1673-1506.2019.06.004
文献标志码:
A
摘要:
前人关于源-汇体系的研究主要集中在海相被动大陆边缘盆地和陆相伸展盆地中,而对走滑型源-汇体系研究较少。本文以辽中南洼旅大16-3地区为例,综合钻井和地震资料系统分析该区走滑型源-汇体系发育特征及沉积响应。研究表明:研究区源-汇体系的形成和演化受走滑作用控制,表现为增压型走滑转换带控制了局部物源体系的发育,释压型走滑转换带控制了有利汇聚体系的形成,走滑水平位移造成源-汇体系的横向错动。局部物源体系和有利汇聚体系的耦合控制了旅大16-3地区东三段砂体富集,源-汇体系横向错动造成该区东三段砂体迁移叠覆且期次明显。本文研究成果有力支持了旅大16-3油田的勘探评价,对于走滑相关沉积盆地源-汇体系及砂体预测研究具有一定借鉴意义。
Abstract:
Previous studies on the source-sink systems mainly focused on the marine passive continental marginal basins and the continental extensional basins, and the studies have been rarely conducted on the strike-slip source-sink system. Taking the LD16-3 area of the southern Liaozhong sag as an example, this paper analyzes the development characteristics and sedimentation response of the strike-slip source-sink system in this area by comprehensively applying the drilling and seismic data. The research suggests that the formation and evolution of source-sink system in this study area are controlled by the strike-slip action, appearing as the development of regional source system dominated by supercharged strike-slip transition zone, the pressure-release strike-slip transition zone controls the formation of favorable convergence system, and the strike-slip horizontal displacement causes the lateral displacement of source-sink system. The coupling of the regional source system and the favorable convergence system controlled the sand body enrichment in Ed3 of the LD16-3 area. The lateral displacement of source-sink system caused the migration and superimposition of sand bodies in Ed3, and the periods were obvious. The research results in this paper strongly support the exploration evaluation of the LD16-3 oilfield, which has a certain reference significance for the source-sink system and sand body prediction researches of the strike-slip related sedimentary basin.

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备注/Memo

备注/Memo:
*“十三五”国家科技重大专项课题“渤海海域勘探新领域及关键技术研究(编号:2016ZX05024-003)”部分研究成果。 第一作者简介: 宛良伟,男,硕士,工程师,毕业于中国地质大学(武汉),主要从事油气勘探研究工作。地址:天津市滨海新区海川路2121号渤海石油管理局B座(邮编:300459)。E-mail:yuanlw@cnooc.com.cn。
更新日期/Last Update: 1900-01-01