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作 者:YUE Shanshan FAN Xiaomin HUANG Buzhou
机构地区:[1]College of Geo-Exploration Science and Technology,Jilin University
出 处:《Global Geology》2019年第3期209-216,共8页世界地质(英文版)
摘 要:In Mesozoic-Cenozoic faulted basin in the periphery of Daqing exploration area, the clastic reservoirs mainly consist of siltstone and gravel-bearing sandstone. The electrical conductivity of the reservoirs is complicated due to the complex pore structures, which cannot be accurately interpreted with commonly used model. In order to solve the problem, a three-water model has been applied in this study based on in-depth analysis of the conductive mechanism of rocks in the explored area, and favorable application results are achieved.In Mesozoic-Cenozoic faulted basin in the periphery of Daqing exploration area, the clastic reservoirs mainly consist of siltstone and gravel-bearing sandstone. The electrical conductivity of the reservoirs is complicated due to the complex pore structures, which cannot be accurately interpreted with commonly used model. In order to solve the problem, a three-water model has been applied in this study based on in-depth analysis of the conductive mechanism of rocks in the explored area, and favorable application results are achieved.
关 键 词:DAQING exploration area MESOZOIC-CENOZOIC faulted BASIN COMPLEX pore structures CEMENTATION INDEX saturation INDEX
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