贵州碳酸盐岩地表堆积物的地质特征及其演化

Geological characteristics and evolution of the surface deposit of Guizhou carbonate rock

碳酸盐岩地表堆积物是岩溶作用后在特殊气候条件下进一步演化的产物 ,因受岩溶作用使其具有独特的地质特征。本文从野外调查入手 ,结合试验资料来研究它的地质特征 ,认为是岩溶作用奠定了这些独特地质特征的基础 ,后期的改造作用对某些地质特征的形成有一定的影响。

The surface deposit of carbonate rock is a product that carbonate rock evolvs further in special climate. Because of karst effect it gets its own geological characteristics. This paper studied the geological characteristics of the surface deposit with field survey and experimental materials. The writer believed that karst offect is the foundation of these characteristics and further evolution had an effect on its formation in some degree.