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
布(集中
布于
峰峰
和
马家
段)。