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    东海陆架盆地形成演化及油气成藏关键地质问题

    钟锴 朱伟林 高顺莉 付晓伟

    钟锴, 朱伟林, 高顺莉, 付晓伟, 2018. 东海陆架盆地形成演化及油气成藏关键地质问题. 地球科学, 43(10): 3485-3497. doi: 10.3799/dqkx.2018.282
    引用本文: 钟锴, 朱伟林, 高顺莉, 付晓伟, 2018. 东海陆架盆地形成演化及油气成藏关键地质问题. 地球科学, 43(10): 3485-3497. doi: 10.3799/dqkx.2018.282
    Zhong Kai, Zhu Weilin, Gao Shunli, Fu Xiaowei, 2018. Key Geological Questions of the Formation and Evolution and Hydrocarbon Accumulation of the East China Sea Shelf Basin. Earth Science, 43(10): 3485-3497. doi: 10.3799/dqkx.2018.282
    Citation: Zhong Kai, Zhu Weilin, Gao Shunli, Fu Xiaowei, 2018. Key Geological Questions of the Formation and Evolution and Hydrocarbon Accumulation of the East China Sea Shelf Basin. Earth Science, 43(10): 3485-3497. doi: 10.3799/dqkx.2018.282

    东海陆架盆地形成演化及油气成藏关键地质问题

    doi: 10.3799/dqkx.2018.282
    基金项目: 

    国家科技重大专项 2016ZX05027-001-008

    海洋地质国家重点实验室自主课题 MG20180101

    国家自然科学基金项目 41702228

    详细信息
      作者简介:

      钟锴(1974-), 男, 教授级高工, 主要从事石油地质研究

      通讯作者:

      朱伟林

    • 中图分类号: P541

    Key Geological Questions of the Formation and Evolution and Hydrocarbon Accumulation of the East China Sea Shelf Basin

    • 摘要: 东海陆架盆地是中国近海规模最大的边缘海盆地,历次资源评价均认为其具有丰富的油气资源潜力,但迄今为止,其油气探明程度仍相对较低.因此,有必要对东海陆架盆地从区域构造背景、盆地形成机制到烃源潜力、沉积储层等油气成藏关键问题展开全面的重新研究和认识.通过对东海及其周缘构造单元基础地质资料、研究现状及存在问题的梳理,提出东海陆架盆地中生代盆地原型及其与周边区域构造演化、晚中生代-新生代裂谷盆地差异演化及其成因、沉积充填特征及其控制因素是研究东海陆架盆地形成演化的3个关键的科学问题.因各次级沉降单元差异演化,造成各区域油气成藏的关键地质要素也存在明显差异,其中储层因素是以始新统-渐新统沉积为主的东部坳陷带油气成藏的关键,而烃源岩条件是解答古新统-始新统沉积为主的西部坳陷带油气成藏的基础性问题.

       

    • 图  1  东海陆架盆地构造划分

      ①昆山凹陷; ②金山北凹陷; ③金山南凹陷; ④钱塘凹陷; ⑤椒江凹陷; ⑥丽水凹陷; ⑦澎佳屿凹陷.长江坳陷包括昆山凹陷、金山北凹陷及金山南凹陷; 东部坳陷带东侧控盆断裂因后期强烈构造反转地震剖面难以识别, 未标识为断裂, 而改用构造单元界线

      Fig.  1.  Division of tectonic units of East China Sea Basin

      图  2  东海中-新生代盆地综合柱状图

      西部坳陷带中-南部包括钱塘凹陷、丽水凹陷、椒江凹陷及福州凹陷; 西部坳陷带北部限于长江坳陷; 东部坳陷带包括福江凹陷、西湖凹陷及钓北凹陷

      Fig.  2.  Comprehensive Mesozoic-Cenozoic stratigraphic column of East China Sea Basin

      图  3  中国近海海域中生代地层分布及地层对比

      Fig.  3.  Distributions of Mesozoic stratigraphy and stratigraphic correlation in China offshore region

      图  4  东海新生代盆地及其台西盆地差异演化特征

      Fig.  4.  The differential evolution features of Cenozoic East China Sea Basin and western Taiwan Basin

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