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OALib Journal期刊
ISSN: 2333-9721
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武威盆地石炭系沉积环境及含油气远景
Keywords: 沉积环境,含油气远景,石炭系,武威盆地
Abstract:
？武威盆地发育厚度近千米的石炭系，具东厚西薄的特点，是一套海陆交互相碎屑岩、碳酸盐岩及含煤沉积。早石炭世早期前黑山组沉积时期，仅在盆地南部接受沉积，厚度为100～150m，气候炎热干旱，以滨浅海和咸化泻湖环境为主，主要沉积了杂色碎屑岩，夹白云岩和石膏沉积，生油能力差；下石炭统上段臭牛沟组—上石炭统靖远组、羊虎沟组、太原组沉积时期，气候温暖湿润，海侵范围扩大，盆地内均有沉积，厚度为300~800m，为滨浅海、滨海沼泽、淡化泻湖、三角洲环境，形成了暗色泥岩、页岩、炭质泥岩、灰岩烃源岩，盆地周缘石炭系烃源岩有机质丰度较高，属中等—好烃源岩，是盆地内主要的生油气源岩，发育自生自储式生储盖组合。综合分析表明武威盆地是一个有潜力的含油气盆地。
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