It's a residual mountain(unaka) which were a set of thrust blocks under the erosion unconformity.It's reservoir pore space is a fracture-vug-pore system of Ordovician carbonate karst.
该气藏的构造为道冲构造侵
而成的残丘山,储集体为奥陶
碳酸盐岩溶
孔体,流体呈层状
布(集中布于奥陶
组和上马家沟组上段)。
It's a residual mountain(unaka) which were a set of thrust blocks under the erosion unconformity.It's reservoir pore space is a fracture-vug-pore system of Ordovician carbonate karst.
该气藏的构造为道冲构造侵而成的残丘山,储集体为奥陶碳酸盐岩溶孔体,流体呈层状布(集中布于奥陶组和上马家沟组上段)。
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