巴彦浩特盆地石炭系储层特征研究  

Reservoir Characteristics of Carboniferous System in Bayanhaote Basin

作　　者：盛双占 SHENG Shuang-zhan(Northwest University, Shaanxi Xi'an 710069, China)

机构地区：[1]西北大学,陕西西安710069

出　　处：《辽宁化工》2019年第3期297-298,共2页Liaoning Chemical Industry

摘　　要：巴彦浩特盆地石炭系储层较发育,潜在的储层岩石类型主要有碎屑岩(砂岩)、碳酸盐岩。碳酸盐岩主要分布于下石炭统,砂岩主要分布于上石炭统。研究区石炭系储层孔隙发育,储层物性较差。成岩作用对储层的物性影响较大。Carboniferous reservoirs are well developed in Bayanhaote Basin. The potential reservoir rock types are mainly sandstone and carbonate rocks. Carbonate rocks are mainly distributed in lower carboniferous system and sandstone rocks are mainly distributed in upper carboniferous system. Carboniferous reservoirs in the study area have well developed pore and poor reservoir physical properties. Diagenesis has a great influence on the physical properties of reservoirs.

关 键 词：石炭系 孔隙 物性 

分 类 号：TE122[石油与天然气工程—油气勘探]