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OALib Journal期刊
ISSN: 2333-9721
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琼东南盆地崖北凹陷崖城组沉积相及煤系烃源岩分布
Keywords: 崖北凹陷,崖城组,煤系,烃源岩,琼东南盆地
Abstract:
？崖北凹陷主力烃源岩是崖城组煤系烃源岩，而煤系的分布受控于沉积相带。为弄清煤系烃源岩分布特征，为油气勘探工作提供参考，通过对区域地质背景、古生物、岩性组合、水动力条件、古地形及与现代沉积类比等综合分析，指出崖北凹陷崖城组主要发育潮坪—潟湖沉积体系。崖城组沉积时期，潮坪之上地势宽广、平坦，并生长着蕨类和红树林等高等植物，有利于煤系的形成和聚集;而凹陷内相对封闭的水动力条件又有利于煤系的保存。因此，潮坪具备了煤系形成、聚集和保存的有利条件，是发育煤系烃源岩的有利沉积相带。崖北凹陷内的潮坪主要发育在南部和东南部缓坡带，其中东南部缓坡带崖城组埋藏深，有机质热演化程度高，推测其已生成油气。
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