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.
出处
《贵州师范大学学报（自然科学版）》
CAS
2004年第2期24-26,共3页
Journal of Guizhou Normal University：Natural Sciences
关键词
岩溶洞穴
岩溶地貌
洞穴沉积
地貌分期
karst cave
cave accumulation
division of different periods for the landform
Guizhou
