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珠江口盆地白云凹陷古近系沉积相类型

李成海 王家豪 柳保军 苏奥 徐东浩 罗泉源 刘姗 牟川

李成海, 王家豪, 柳保军, 苏奥, 徐东浩, 罗泉源, 刘姗, 牟川. 珠江口盆地白云凹陷古近系沉积相类型[J]. 沉积学报, 2014, 32(6): 1162-1170.
引用本文: 李成海, 王家豪, 柳保军, 苏奥, 徐东浩, 罗泉源, 刘姗, 牟川. 珠江口盆地白云凹陷古近系沉积相类型[J]. 沉积学报, 2014, 32(6): 1162-1170.
LI Cheng-hai, WANG Jia-hao, LIU Bao-jun, SU Ao, XU Dong-hao, LUO Quan-yuan, LIU Shan, MU Chuan. Types and Distribution of the Paleogene Sedimentary Facies in Baiyun Depression of Pearl River Mouth Basin[J]. Acta Sedimentologica Sinica, 2014, 32(6): 1162-1170.
Citation: LI Cheng-hai, WANG Jia-hao, LIU Bao-jun, SU Ao, XU Dong-hao, LUO Quan-yuan, LIU Shan, MU Chuan. Types and Distribution of the Paleogene Sedimentary Facies in Baiyun Depression of Pearl River Mouth Basin[J]. Acta Sedimentologica Sinica, 2014, 32(6): 1162-1170.

珠江口盆地白云凹陷古近系沉积相类型

详细信息
    作者简介:

    李成海 男 1987年出生 硕士 沉积及层序地层 E-mail: li_chenghai_cool@126.com

  • 中图分类号: TE122.2

Types and Distribution of the Paleogene Sedimentary Facies in Baiyun Depression of Pearl River Mouth Basin

  • 摘要: 以珠江口盆地白云凹陷的钻井和地震资料为基础,根据测井相、地震相综合分析白云凹陷文昌组与恩平组主要层序的沉积相发育演化特征.通过有限的单井资料在白云凹陷共识别出了三角洲相、扇三角洲相及湖泊相三种沉积相;三角洲沉积相在测井曲线上表现为从下至上由细变粗的反旋回,局部出现次一级的正旋回;扇三角洲沉积相测井曲线整体表现为从下至上由细变粗的反旋回及次一级的反旋回;湖泊沉积相表现为以泥岩沉积为主,局部夹有砂坝或碳酸盐滩坝.研究区发育9种地震相类型,地震相证据充足,为研究沉积相发育规律提供了可靠的依据.研究表明盆地的持续沉降造就了白云凹陷深湖相发育时间长,形成厚层烃源岩;受番禺低隆起影响,白云凹陷北坡缓坡带发育三角洲相,在西南至南部陡坡带发育扇三角洲相,部分三角洲的发育具有继承性.
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  • [1] 李忠.  “从最高到最深”—从第17届国际沉积学大会看沉积学研究前沿 . 沉积学报, 2006, (6): 928-933.
    [2] 李 忠.  “从最高到最深”—从第17届国际沉积学大会看沉积学研究前沿 . 沉积学报, 2006, 24(06): 928-933.
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出版历程
  • 收稿日期:  2013-10-08
  • 修回日期:  2013-12-16
  • 刊出日期:  2014-12-10

目录

    珠江口盆地白云凹陷古近系沉积相类型

      作者简介:

      李成海 男 1987年出生 硕士 沉积及层序地层 E-mail: li_chenghai_cool@126.com

    • 中图分类号: TE122.2

    摘要: 以珠江口盆地白云凹陷的钻井和地震资料为基础,根据测井相、地震相综合分析白云凹陷文昌组与恩平组主要层序的沉积相发育演化特征.通过有限的单井资料在白云凹陷共识别出了三角洲相、扇三角洲相及湖泊相三种沉积相;三角洲沉积相在测井曲线上表现为从下至上由细变粗的反旋回,局部出现次一级的正旋回;扇三角洲沉积相测井曲线整体表现为从下至上由细变粗的反旋回及次一级的反旋回;湖泊沉积相表现为以泥岩沉积为主,局部夹有砂坝或碳酸盐滩坝.研究区发育9种地震相类型,地震相证据充足,为研究沉积相发育规律提供了可靠的依据.研究表明盆地的持续沉降造就了白云凹陷深湖相发育时间长,形成厚层烃源岩;受番禺低隆起影响,白云凹陷北坡缓坡带发育三角洲相,在西南至南部陡坡带发育扇三角洲相,部分三角洲的发育具有继承性.

    English Abstract

    李成海, 王家豪, 柳保军, 苏奥, 徐东浩, 罗泉源, 刘姗, 牟川. 珠江口盆地白云凹陷古近系沉积相类型[J]. 沉积学报, 2014, 32(6): 1162-1170.
    引用本文: 李成海, 王家豪, 柳保军, 苏奥, 徐东浩, 罗泉源, 刘姗, 牟川. 珠江口盆地白云凹陷古近系沉积相类型[J]. 沉积学报, 2014, 32(6): 1162-1170.
    LI Cheng-hai, WANG Jia-hao, LIU Bao-jun, SU Ao, XU Dong-hao, LUO Quan-yuan, LIU Shan, MU Chuan. Types and Distribution of the Paleogene Sedimentary Facies in Baiyun Depression of Pearl River Mouth Basin[J]. Acta Sedimentologica Sinica, 2014, 32(6): 1162-1170.
    Citation: LI Cheng-hai, WANG Jia-hao, LIU Bao-jun, SU Ao, XU Dong-hao, LUO Quan-yuan, LIU Shan, MU Chuan. Types and Distribution of the Paleogene Sedimentary Facies in Baiyun Depression of Pearl River Mouth Basin[J]. Acta Sedimentologica Sinica, 2014, 32(6): 1162-1170.
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