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OALib Journal期刊
ISSN: 2333-9721
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塔里木盆地奥陶系碳酸盐岩“非串珠状”缝洞型储层类型及成因
Keywords: 碳酸盐岩,&ldquo,非串珠状&rdquo,缝洞型储层,裂缝,古河道,塔里木盆地
Abstract:
？塔里木盆地奥陶系碳酸盐岩中“非串珠状”缝洞型储层经钻探已取得较好效果，但目前针对其储层类型及成因的研究较少。根据碳酸盐岩缝洞储集体发育程度及受风化壳和裂缝的影响程度，将在地震剖面上表现为“非串珠状”反射的缝洞型储层划分为3种类型，分别是内幕缝洞体规模较小的缝洞型储层、距风化壳较近的缝洞型储层以及裂缝型储层，进行正演模拟，并与实钻资料结合，详细探讨各自的地震反射特征和地质成因。
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