黔东万山－湖南新晃地区的寒武系中风暴沉积发育。风暴沉积的岩石类型主要是砾屑石灰岩和砂屑石灰岩，砾屑石灰岩从细砾屑石灰岩到巨砾屑石灰岩均有，但以中砾屑石灰岩最多，砾屑大都呈板状，但有的呈近等轴状。其排列方式呈平行状和迭瓦状。砂屑石灰岩具递变层理、平行层理、丘状层理、单向交错层理等。砾屑石灰岩和砂屑石灰岩夹于大套暗色中薄层碳酸盐岩中，为斜坡环境中的风暴沉积。 Cambrian Mesozoic Sedimentary Deposition in the Wanshan Mountains, Eastern Guizhou Province - Xinhuang Region, Hunan Province. The types of rocks deposited by the storm are mainly gravelly limestone and litter limestone, both from gravelly limestone and gravelly limestone, but most of the conglomerate limestone and gravel are mostly plate-shaped, but some are Nearly equiaxed. The arrangement was parallel and Diego-like shape. Sandstone limestone with graded bedding, parallel bedding, mound bedding, one-way staggered bedding and so on. Gravel limestone and sandstone limestone are sandwiched between large sets of dark-medium thin-bedded carbonate rocks and are storm deposits in a ramp environment.