【摘 要】
:
上白垩统土伦阶Madingo组烃源岩是下刚果盆地漂移期的主力海相烃源岩,有机岩石学和分子地化特征分析表明该套烃源岩主要包括海相内源型和海相混合生源型两种成因类型.本文采用微观沉积学研究方法,从古地理环境、陆源营养供给、古生产力和保存条件等方面入手,对下刚果盆地Madingo组烃源岩发育的控制因素开展了研究,明确了陆架内洼槽及其内部盐控微盆的局限古地理环境、陆源营养物质的间歇性悬浮供给方式是该盆地Madingo组优质海相烃源岩发育的主控因素;在此基础上,建立了具有陆源营养物质输入的河流-陆架内洼槽局限环境海
【机 构】
:
中国海洋石油国际有限公司北京 100028
论文部分内容阅读
上白垩统土伦阶Madingo组烃源岩是下刚果盆地漂移期的主力海相烃源岩,有机岩石学和分子地化特征分析表明该套烃源岩主要包括海相内源型和海相混合生源型两种成因类型.本文采用微观沉积学研究方法,从古地理环境、陆源营养供给、古生产力和保存条件等方面入手,对下刚果盆地Madingo组烃源岩发育的控制因素开展了研究,明确了陆架内洼槽及其内部盐控微盆的局限古地理环境、陆源营养物质的间歇性悬浮供给方式是该盆地Madingo组优质海相烃源岩发育的主控因素;在此基础上,建立了具有陆源营养物质输入的河流-陆架内洼槽局限环境海相烃源岩发育模式,指出陆架内洼槽是该盆地Madingo组优质海相烃源岩发育区,Madingo组有效生烃灶的展布控制了该盆地古近系—新近系油气田的差异分布,这种“源控成藏”的认识可有效指导该领域下一步勘探工作.
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