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    东海丽水凹陷早新生代沉积特征及物源演化

    刘正华 侯元立 陈淑慧 廖凯飞 邵磊 朱伟林

    刘正华, 侯元立, 陈淑慧, 廖凯飞, 邵磊, 朱伟林, 2022. 东海丽水凹陷早新生代沉积特征及物源演化. 地球科学, 47(7): 2562-2572. doi: 10.3799/dqkx.2022.244
    引用本文: 刘正华, 侯元立, 陈淑慧, 廖凯飞, 邵磊, 朱伟林, 2022. 东海丽水凹陷早新生代沉积特征及物源演化. 地球科学, 47(7): 2562-2572. doi: 10.3799/dqkx.2022.244
    Liu Zhenghua, Hou Yuanli, Chen Shuhui, Liao Kaifei, Shao Lei, Zhu Weilin, 2022. Early Cenozoic Sedimentary Characteristics and Provenance Evolution of Lishui Depression, East China Sea. Earth Science, 47(7): 2562-2572. doi: 10.3799/dqkx.2022.244
    Citation: Liu Zhenghua, Hou Yuanli, Chen Shuhui, Liao Kaifei, Shao Lei, Zhu Weilin, 2022. Early Cenozoic Sedimentary Characteristics and Provenance Evolution of Lishui Depression, East China Sea. Earth Science, 47(7): 2562-2572. doi: 10.3799/dqkx.2022.244

    东海丽水凹陷早新生代沉积特征及物源演化

    doi: 10.3799/dqkx.2022.244
    基金项目: 

    国家科技重大计划 2018YFE0202400

    国家自然科学基金项目 42076066

    国家自然科学基金项目 92055203

    详细信息
      作者简介:

      刘正华(1978-),女,助理研究员,博士,从事油气成藏、沉积学和地球化学研究. ORCID:0000-0001-9839-1967. E-mail:liuzhtongji@tongji.edu.cn

    • 中图分类号: P618.13

    Early Cenozoic Sedimentary Characteristics and Provenance Evolution of Lishui Depression, East China Sea

    • 摘要: 东海陆架盆地新生代发育大型弧后盆地,接受了海相及陆相沉积,油气资源丰富,勘探前景广阔. 其中,丽水凹陷发育了古新统‒始新统扇三角洲、河流三角洲及滨浅海相沉积,其沉积环境及沉积物源研究一直存在争议. 通过古生物学和碎屑锆石U-Pb年龄谱系综合分析,对丽水凹陷古新统‒始新统沉积环境及潜在源区进行系统的源汇对比研究. 结果表明,丽水凹陷古新统及下中始新统以滨浅海相为特征,凹陷东侧海水较深,沉积物主要来自周边燕山期岩浆岩古隆起. 然而,凹陷东、西次凹在沉积物源上存在明显差异,西次凹沉积物锆石U-Pb年龄谱系仅发育燕山期单峰,东次凹还存在明显的印支期物源;特别是进入始新世,东次凹温州组物源发生明显改变,出现大量古老锆石,沉积物来自北部渔山低隆起,显示该时期在凹陷北侧发育较大规模的三角洲沉积. 晚始新世,由于玉泉运动,丽水凹陷发生隆升剥蚀,直到中新世再次接受沉积. 丽水凹陷古新统‒始新统以海陆过渡环境为主,有利于烃源岩及储集体的发育,具有良好的油气勘探潜力.

       

    • 图  1  东海陆架盆地构造区划图及研究样品分布

      LSS. 丽水凹陷;JJS. 椒江凹陷;XHS. 西湖凹陷;FZS. 福州凹陷;DBS. 钓北凹陷;QTS. 钱塘凹陷

      Fig.  1.  Simplified geological map and sample location of the East China Sea Shelf Basin

      图  2  丽水凹陷古新‒始新世地层构造演化综合图

      Fig.  2.  Paleocene-Eocene stratigraphic framework of the Lishui Depression

      图  3  丽水凹陷基底及周边潜在源区锆石年龄谱系特征

      Fig.  3.  Zircon U-Pb spectra of the Lishui Depression basement and potential source terranes

      图  4  丽水凹陷的海洋化石记录和海平面变化

      Fig.  4.  Marine fossil records and sea-level changes of the Lishui Depression

      图  5  丽水凹陷白垩纪到晚始新世样品的碎屑锆石U-Pb年龄谱图(n代表有效数据点)

      Fig.  5.  Detrital zircon U-Pb age spectra of Cretaceous to Late Eocene samples from the Lishui Depression (n represents effective analyses)

      图  6  碎屑锆石Th/U比值与U-Pb年龄分布

      Fig.  6.  Distribution of Th/U ratios and U-Pb ages of detrital zircon

      图  7  古新世到始新世古环境演化阶段

      Fig.  7.  Evolutionary stages of sedimentary environment from Paleocene to Eocene

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    出版历程
    • 收稿日期:  2022-05-27
    • 网络出版日期:  2022-07-29
    • 刊出日期:  2022-07-25

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