奥陶系

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,为奥陶系碳酸盐岩溶蚀缝洞孔系,流呈层状分(中分于奥陶系峰峰组和马家沟组段)。