摘要：

早-中三叠世贵阳花溪地区位于浅水碳酸盐台地向深水盆地的过渡带，各沉积体系域特征明显，特别是低水位期碳酸盐角砾岩楔发育。野外调查发现研究区共发育4期低水位碳酸盐角砾岩楔，说明该区在早-中三叠世至少经历了4次明显的海平面变化。碳酸盐角砾岩楔的位置迁移反应了台地边缘位置的迁移和海平面相对变化的大小，其中谷立角砾岩舌相对于其他角砾岩楔向台地方向延伸距离最远，代表了台地边缘位置向台地方向迁移的距离最远，张家湾角砾岩楔代表了安尼初期的海平面快速下降。通过角砾岩楔的沉积特征和各岩石地层单元的几何接触关系判断出该区碳酸盐台地前缘演化过程：缓斜坡型台缘→沉积型台缘→礁镶跌积型台缘。

Abstract:

Huaxi area of Guiyang was located in the transitional belt from shallow-water carbonate platform to deep-water basin during the Early–Middle Triassic, and each sedimentary systems tract has its own characteristics especially the carbonate breccia wedge of lowstand systems tract(LST). The field investigation indicates that there are four times of carbonate breccia wedge of LST, which reflect this area experienced at least four significant sea level changes in the Early –Middle Triassic. The migration of carbonate breccia wedge also reflects the shifting of the platform margin and the relative sea level changes. Among them, the Guli breccia  wedge extended the farest distance to the platform, which represents that the platform margin shifted to the platform for the farest distance. The Zhangjiawan breccia wedge represents the fast sea level falling in the Early Anisian. In addition, this paper reconstructed the evolution of cabonate platform margin based on the analyses of  the depositional characteristics of the breccia wedge and the geometric relationship of each lithostratigraphic unit: ramp platform margin→depositional platform margin→reef by-pass margin.