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成的残丘山,储集
为
陶系碳酸盐岩溶
缝
系,流
呈层状分布(集中分布于
陶系峰峰组和上马家沟组上段)。