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    南海始新世海相地层分布及油气地质意义

    张浩 邵磊 张功成 陈淑慧 吴国瑄

    张浩, 邵磊, 张功成, 陈淑慧, 吴国瑄, 2015. 南海始新世海相地层分布及油气地质意义. 地球科学, 40(4): 660-670. doi: 10.3799/dqkx.2015.053
    引用本文: 张浩, 邵磊, 张功成, 陈淑慧, 吴国瑄, 2015. 南海始新世海相地层分布及油气地质意义. 地球科学, 40(4): 660-670. doi: 10.3799/dqkx.2015.053
    Zhang Hao, Shao Lei, Zhang Gongcheng, Chen Shuhui, Wu Guoxuan, 2015. Distribution and Petroleum Geologic Significance of Eocene Marine Strata in the South China Sea. Earth Science, 40(4): 660-670. doi: 10.3799/dqkx.2015.053
    Citation: Zhang Hao, Shao Lei, Zhang Gongcheng, Chen Shuhui, Wu Guoxuan, 2015. Distribution and Petroleum Geologic Significance of Eocene Marine Strata in the South China Sea. Earth Science, 40(4): 660-670. doi: 10.3799/dqkx.2015.053

    南海始新世海相地层分布及油气地质意义

    doi: 10.3799/dqkx.2015.053
    基金项目: 

    国家自然科学基金项目 91128207

    国家自然科学基金项目 40976023

    国家科技重大专项 2011ZX05025-006-02

    详细信息
      作者简介:

      张浩(1990-), 男, 硕士, 主要从事沉积学研究.E-mail: 90_zhang_hao@tongji.edu.cn

    • 中图分类号: TE121

    Distribution and Petroleum Geologic Significance of Eocene Marine Strata in the South China Sea

    • 摘要: 采用古生态学及沉积学方法, 对南海北部深水区BY7-1-1井及L29井特定层段进行细致研究.通过有孔虫、孢粉藻类分析及沉积学分析, 证实南海北部白云深水区在晚始新世即出现滨浅海相沉积环境, 确定了南海北部最早接受海相沉积的时间.始新世海相地层在南海北部主要分布在台西及台西南盆地中, 并在晚始新世扩展到珠江口盆地白云凹陷.在南部分布较广, 曾母盆地、北康盆地、礼乐盆地及巴拉望盆地中均有始新世海相地层分布.南海始新世海相地层的分布受制于新南海扩张及古南海的消退, 以晚始新世为时间节点发生显著变化, 总体上分布范围增大, 反映该时期南海拉张和断裂活动的加剧.南海始新世海相地层具有良好的油气潜力, 在部分盆地中形成了优质的烃源岩与储层, 珠江口盆地白云深水区晚始新世海相地层的发现, 对南海深水海相油气勘探具有积极的参考作用.

       

    • 图  1  南海海域新生代沉积盆地分布及井位(底图据中国地图,中国地图出版社,2013)

      Fig.  1.  Distribution of Cenozoic sedimentary basins and well locations in South China Sea

      图  2  BY7-1-1井地层划分

      Fig.  2.  Stratigraphic division of well BY7-1-1

      图  3  L29井分析层段浮游藻类

      1.Pediastrum spp.;2.Spherical algae;3.Apteodinium spp.;4.Cleistosphaeridium diversisposum;5.Cleistosphaeridium spp.;6.Cordosphaeridium exsilimurum;7.C. gracile;8.C. inodes;9.Cordosphaeridium spp.;10.Homotryblium plectilum;11.Homotryblium tenuispinosum;12.Homotryblium spp.;13.Hystrichokolpoma spp.;14.Hystrichosphaeridium tubiferum;15.Lingoludinium machaerophorum;16.Polysphaeridium zoharyi;17.Spiniferites spp.;18.Systematophora ancyrea;19.S. placacantha

      Fig.  3.  Planktonic algae schema of analytic interval, well L29

      图  4  L29井分析层段有机屑类型变化特征

      Fig.  4.  Change characteristics of organic detrital components of analytic interval, well L29

      图  5  南海始新世海相地层分布演化(底图据中国地图,中国地图出版社,2013)

      a.早-中始新世;b.晚始新世-早渐新世;据许淑梅等(2013)修改

      Fig.  5.  Distribution and Evolution of Eocene marine-phase sedimentary strata in South China Sea

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    • 收稿日期:  2014-09-21
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