Member 2 of Upper Triassic Xujiahe Formation is a set of debris-feldspar and feldspar-quartz sandstone in the Yingshan structure. Based on the cores, the flake observation and physical properties data of the reservoir in the T3x2, this paper indicates that the 2nd member belongs to the front-delta deposition. The main reservoir sandy bodies have deposited in subaqueous distributary channel and distributary mouth bar with intergranular pore and intragranular pores as reservoir space. The reservoir is a cracked-porous type with low porosity and low permeability. The reservoir’s development is influenced by both sedimentary facies and diagenesis.