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南海北缘陆相断陷盆地优质烃源岩发育机制:以珠江口盆地顺德凹陷始新统文昌组为例*
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高梦天, 尤丽, 胡高伟, 龚宇, 李彦丽, 陈亚兵, 冯琦, 韩骏威, 刘国麟 |
Formative mechanisms of high-quality source rocks in continental fault basin of northern South China Sea: a case study from the Eocene Wenchang Formation in Shunde sag,Pearl River Mouth Basin
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GAO Mengtian , YOU Li , HU Gaowei, GONG Yu, LI Yanli, CHEN Yabing, FENG Qi, HAN Junwei, LIU Guolin
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珠江口盆地顺德凹陷区域地质背景 a—珠江口盆地构造单元划分纲要图(据Guan et al ., 2016修改);b—顺德凹陷始新统文昌组二段页岩相带及厚度分布图;c—顺德凹陷构造—地层特征地质剖面(Line A) |
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