摘要
In Huangguoshu-Tianxingqiao area, Anshun, Guizhou Province, the dolomite of the Lower Triassic Anshun Formation was widely exposed, and a contiguous Water Stone Forest was developed. The Anshun Formation was developed on the transitional zone between the Triassic deep - sea basin and platform margin where marine transgression happened frequently, and large tepee structures were well developed on the exposed surface of the ancient coastal. In this paper, combining field visits and previous data, the authors attempt to study the control action of the large tepee structure to the formation and evolution of karst stone forest in this area.