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    莺歌海盆地浅海环境下烃源岩有机质形成机制

    徐新德 杨计海 刘海钰 郭潇潇 熊小峰 梁刚

    徐新德, 杨计海, 刘海钰, 郭潇潇, 熊小峰, 梁刚, 2019. 莺歌海盆地浅海环境下烃源岩有机质形成机制. 地球科学, 44(8): 2643-2653. doi: 10.3799/dqkx.2019.091
    引用本文: 徐新德, 杨计海, 刘海钰, 郭潇潇, 熊小峰, 梁刚, 2019. 莺歌海盆地浅海环境下烃源岩有机质形成机制. 地球科学, 44(8): 2643-2653. doi: 10.3799/dqkx.2019.091
    Xu Xinde, Yang Jimei, Liu Haiyu, Guo Xiaoxiao, Xiong Xiaofeng, Liang Gang, 2019. Formation Mechanism of Organic Matter in Source Rocks under Marine Environment in Yinggehai Basin. Earth Science, 44(8): 2643-2653. doi: 10.3799/dqkx.2019.091
    Citation: Xu Xinde, Yang Jimei, Liu Haiyu, Guo Xiaoxiao, Xiong Xiaofeng, Liang Gang, 2019. Formation Mechanism of Organic Matter in Source Rocks under Marine Environment in Yinggehai Basin. Earth Science, 44(8): 2643-2653. doi: 10.3799/dqkx.2019.091

    莺歌海盆地浅海环境下烃源岩有机质形成机制

    doi: 10.3799/dqkx.2019.091
    基金项目: 

    国家“十三五”重大科技专项“莺琼盆地高温高压天然气富集规律与勘探开发关键技术(三期)” 2016ZX05024-005

    详细信息
      作者简介:

      徐新德(1970-), 男, 高级工程师, 硕士, 主要从事油气地球化学与成藏研究工作

    • 中图分类号: P588

    Formation Mechanism of Organic Matter in Source Rocks under Marine Environment in Yinggehai Basin

    • 摘要: 为了解莺歌海盆地海相烃源岩有机质形成机制,本研究引入地球生物学方法正演烃源岩形成过程,弥补盆地样品条件的不足,再结合有机地球化学方法,综合研究莺歌海盆地海相烃源岩有机质形成机制,建立烃源岩发育模式.研究认为:莺歌海盆地中新统发育浅海相烃源岩,有机质类型以Ⅱ2-Ⅲ型为主,为混合型生源母质,现今凹陷内大部分烃源岩处于高熟-过成熟生气阶段.海相烃源岩以古生产力和保存条件为主要控制因素,平面上,莺歌海盆地东方区中新统烃源岩发育条件优于乐东区;纵向上,梅山组可能是有利的烃源层段.研究成果为正确认识莺歌海盆地烃源岩形成机制并准确评价其资源潜力提供了重要依据.

       

    • 图  1  莺歌海盆地构造区划分图及地层柱状图

      Fig.  1.  Sketch map and stratigraphic column map of Yinggehai Basin

      图  2  莺歌海盆地中新统烃源岩有机质丰度评价

      Fig.  2.  Assessment of organic matter abundance of Miocene source rocks in the Yinggehai Basin

      图  3  莺歌海盆地中新统烃源岩有机质类型划分

      Fig.  3.  Classification of organic matter types of Miocene source rocks in theYinggehai Basin

      图  4  莺歌海盆地中新统烃源岩饱和色谱及m/z191、m/z217质量色谱

      Fig.  4.  The chromatogram of the saturated hydrocarbon, mass chromatogram of terpenes(m/z191) and steranes (m/z217)from Miocene source rocks in the Yinggehai Basin

      图  5  莺歌海盆地Z11-1-1井孢粉分布

      Fig.  5.  Variation of the sporopollen in Well Z11-1-1

      图  6  莺歌海盆地中新统烃源岩显微组成三角图

      Fig.  6.  Ternary diagram of maceral composition of Miocene source rocks in the Yinggehai Basin

      图  7  莺歌海盆地中新统烃源岩主量元素Al2O3与P2O5交汇图

      Fig.  7.  Intersection map of major elements Al2O3 and P2O5 of Miocene source rocks in Yinggehai Basin

      图  8  莺歌海盆地黄流组海相泥岩TOC与氧指数的相关图

      Fig.  8.  Correlation diagram of organic matter abundance and oxygen index of marine mudstone in the Huangliu formation, Yinggehai Basin

      图  9  莺歌海盆地东方区与乐东区有机屑组分A-P-E三元图

      Fig.  9.  A-P-E ternary map of organic debris components in the Dongfang area and Ledong area of Yinggehai Basin

      图  10  莺-琼盆地海平面变化及干酪根碳同位素分布特征

      Fig.  10.  Distribution characteristic map of the relative change of sea-level and carbon isotope of Kerogen in the Yinggegai-Qiongdongnan Basin

      图  11  莺歌海盆地海相烃源岩发育模式

      Fig.  11.  Model for the development of marine source rock in the Yinggehai Basin

      表  1  莺歌海盆地梅山、三亚组烃源岩有机质丰度统计表

      Table  1.   Statistical table of organic matter abundance of source rocks of Meishan and Sanya formations in Yinggehai Basin

      层位 TOC(%) S1+S2 (mg/g) 氯仿沥青“A”(%) 氢指数HI(mg/g) 成熟度Ro(%) 类型
      梅山组 0.10~3.17 0.02~7.07 0.002~0.098 7~465 0.49~0.75 2型和Ⅲ型
      0.61(192) 0.94(182) 0.046(38) 127(137) 0.66(27)
      三亚组 0.20~1.17 0.06~2.78 0.014 8~0.065 9 13~456 0.61~0.79 2型和Ⅲ型
      0.59(50) 0.79(50) 0.040 2(11) 106(42) 0.72(7)
      注:表中数据格式为最小值-最大值/平均值(样品数).
      下载: 导出CSV
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    • 收稿日期:  2019-01-10
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