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蚀而成的残丘山,储集体为奥陶系
岩溶蚀缝洞孔体系,流体呈层状
布(集中布于奥陶系峰峰组和
沟组段)。
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蚀而成的残丘山,储集体为奥陶系岩溶蚀缝洞孔体系,流体呈层状布(集中布于奥陶系峰峰组和沟组段)。
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