Aiming at Chengdian deep water sandstone in Biyang depression of Nanxiang basin, we analyzed the core, the particle size, thin section, heavy minerals testing materials, structure of sandbody and the geophysical response of sedimentary sandbody, and found that the sub-lacustrine fan is an isolated body with fine and coarse lithology. The result shows: zircons microarea apparent ages of Chengdian sub-lacustrine and Houzhuang delta mainly similarly distribute between 115 Ma and 166 Ma with single peak and the magmatic zircons occupy the main part, with a few metamorphic zircons.