| 岩溶洞穴形态沉积与贵州地貌发育 |
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| 引用本文： | 秦启万,何才华.岩溶洞穴形态沉积与贵州地貌发育[J].贵州师范大学学报(自然科学版),2004,22(2):24-26. |
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| 作者姓名： | 秦启万 何才华 |
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| 作者单位： | 贵州师范大学,地理与生物科学学院,贵州,贵阳,550001;贵州师范大学,地理与生物科学学院,贵州,贵阳,550001 |
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| 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。
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| 关 键 词： | 岩溶洞穴 洞穴沉积 地貌分期 贵州 |
| 文章编号： | 1004-5570(2004)02-0024-03 |
| 修稿时间： | 2004年1月5日 |
Morphological accumulation of karst cave and landform development in Guizhou |
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| QIN Qi-wan,HE Cai-hua.Morphological accumulation of karst cave and landform development in Guizhou[J].Journal of Guizhou Normal University(Natural Sciences),2004,22(2):24-26. |
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| Authors: | QIN Qi-wan HE Cai-hua |
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| Abstract: | 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. |
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| Keywords: | karst cave cave accumulation division of different periods for the landform Guizhou |
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