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
碳酸盐岩溶蚀缝洞孔体,流体呈层状分
(集中分于峰峰组和
马家沟组
)。
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,储集体为碳酸盐岩溶蚀缝洞孔体,流体呈层状分(集中分于峰峰组和马家沟组)。
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