岩溶洞穴形态沉积与贵州地貌发育  

Morphological accumulation of karst cave and landform development in Guizhou

作　　者：秦启万[1] 何才华[1] 

机构地区：[1]贵州师范大学地理与生物科学学院,贵州贵阳550001

出　　处：《贵州师范大学学报（自然科学版）》2004年第2期24-26,共3页Journal of Guizhou Normal University：Natural Sciences

摘　　要：岩溶洞穴是岩溶地貌的组成部分,它与洞外的地貌的形成和发展有着密切的关系,洞穴沉积物常能保存较好的地貌形成的历史印迹,通过对贵州岩溶洞穴沉积特点的分析,就贵州地貌发育演化阶段及分期问题进行了论述和讨论。Being a component of the limestone landform,karst cave has a close relationship with the formation and development of the topographical features outside the cave.The evolution of landform can be well kept by accumulations in the cave.This paper describes and discusses the problems concerning the evolutional stages of different periods for the landform of Guizhou province,by means of analysis on the characteristics of karst cave accumulations.

关 键 词：岩溶洞穴 岩溶地貌 洞穴沉积 地貌分期 

分 类 号：P642.25[天文地球—工程地质学]