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贵州荔波岩溶洞穴发育特征
引用本文:张美良,林玉石,冉景丞,陈会明.贵州荔波岩溶洞穴发育特征[J].中国岩溶,2000,19(1):13-20.
作者姓名:张美良  林玉石  冉景丞  陈会明
作者单位:1. 中国地质科学院岩溶地质研究所、岩溶动力学开放研究实验室,桂林541004
2. 贵州茂兰国家级自然保护区管理处,荔波558400
摘    要:荔波位于云贵高原岩溶向广西岩溶丘陆和孤峰岩溶平原过渡的岩溶斜坡地带。区内岩溶洞穴极其发育,岩溶洞穴(在时空分布上受区域碳酸盐岩地层分布的控制,表现出对地层岩笥的选择笥和洞穴发育的忝层性特点,岩溶洞穴的发育规模、方向明显受断裂、裂隙构造的控制,表现出极强的方向性。本文主要 的形成条件、洞穴空间展布的控制特征以及洞穴沉积物的特征等。论述了区内岩溶洞穴的发育特征。

关 键 词:岩溶洞穴  发育特征  贵州  荔波岩溶洞

THE CHARACTERISTICS OF KARST CAVES DEVELOPMENT IN LIBO, GUIZHOU
Zhang Meiliang,Lin Yushi,Ran Jingcheng and Chen Huiming.THE CHARACTERISTICS OF KARST CAVES DEVELOPMENT IN LIBO, GUIZHOU[J].Carsologica Sinica,2000,19(1):13-20.
Authors:Zhang Meiliang  Lin Yushi  Ran Jingcheng and Chen Huiming
Affiliation:Institute of Karst Geology , CAGS , Guilin 541004, China,Institute of Karst Geology , CAGS , Guilin 541004, China,The Management of Maolan National Nature Reserve, Libo , Guizhou , 558400, China and The Management of Maolan National Nature Reserve, Libo , Guizhou , 558400, China
Abstract:Libo is located in the geomorphological slope zone from the Yunnan-Guizhou plateau to the karst hill and the karst isolated plain of Guangxi. Karst caves develope very well in the area. The distribution of the karst caves are controlled by the spacial distribution of carbonate rocks in the region, which is shown by the selective features to strata or lithology, and the layered characteristics of the karst caves. The size and the orientation of the karst caves are obviously controlled by fractures and fissures. Based on the forming conditions and the controlling factors on the space distribution and the sedimentary-accumulative formations in the caves, the characteristics of the caves development in the area are discussed in this paper.
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