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东海西湖凹陷新生界沉积相的演化
引用本文:林志强,周平.东海西湖凹陷新生界沉积相的演化[J].海洋地质与第四纪地质,1994,14(2):63-70.
作者姓名:林志强  周平
作者单位:上海海洋地质调查局
基金项目:“七五”国家重点科技攻关项目
摘    要:西湖凹陷是东海陆架盆地重点生海气凹陷之一,它在新生代经历断陷,坳陷,区域抬升和区域沉降四个阶段,在纵向序列上表现为二次明显的海侵和一次海退,一次水进和一次水退。由于构造运动的不均匀性,沉积基地的起伏,多物源和水进水退多次旋回,在凹陷不同时期,不同部形成不同的沉答相,这一切与下油气的生成,聚集有着极为密切的关系。

关 键 词:东海  沉积相  油气藏  新生代

EVOLUTION OF CENOZOIC SEDIMENENTARY FACIES OF XIHU DEPRESSION IN THE SHELF BASIN OF THE EAST CHINA SEA
Lin Zhiqing Zhou Ping.EVOLUTION OF CENOZOIC SEDIMENENTARY FACIES OF XIHU DEPRESSION IN THE SHELF BASIN OF THE EAST CHINA SEA[J].Marine Geology & Quaternary Geology,1994,14(2):63-70.
Authors:Lin Zhiqing Zhou Ping
Abstract:Xihu Depression is one of the important petroliferous depressions in the shelf basinof the East China Sea,Its Cenozoic history can be divided into four stages:rifting, de-pressing,regional uplifting and subsiding.Two major transgressions,a regression,a wa-ter-level rise and a fall can be seen in vertical sequence,Because of nonequilibrium of tec-tonic movement,undulating sedimentary base,multiple material sources and multiple cy-cles of water rises and falls,different sedimentary facies accur at different parts of thedepression,Oil and gas generation and accumulation are closely related to the sedimenta-ry facies.
Keywords:East China Sea  Cenozoic sedimentary facies oil and gas  
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