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OALib Journal期刊
ISSN: 2333-9721
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渤海湾盆地歧北次凹超压背景下异常高孔带成因分析与有利储层预测
Keywords: 异常高孔带,致密砂岩,超压,孔隙演化动平衡,歧北次凹
Abstract:
？为了预测渤海湾盆地歧北次凹深层高温、高压背景下，低孔、低渗致密砂岩中有利储层的分布，首先应用储层实测数据研究了储层异常高孔带在纵向上的分布及其成因，然后应用成岩作用数值模拟技术，预测了es下1储层的成岩阶段，结合前人沉积相和超压的研究成果，预测了有利储层的分布。结果表明，歧北凹陷在2300~2740m、3000~3400m、3600~4200m及4400~4950m的深度范围内，发育4个异常高孔带，其成因为大气水淋滤、有机酸溶蚀以及超压对成岩作用的抑制；处于早成岩阶段b期—中成岩阶段a1亚期且有砂体发育的区域，或目前处于中成岩阶段a2亚期但有超压发育，超压可使地史时期形成的次生孔隙保存下来的砂体发育区,是储层发育的有利地区，这些地区位于港东断裂的东部和马棚口地区。？
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