| 桂林地区灰岩洞穴的溶蚀形态 |
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| 引用本文： | 朱学稳.桂林地区灰岩洞穴的溶蚀形态[J].中国岩溶,1982(2):93-103. |
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| 作者姓名： | 朱学稳 |
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| 作者单位： | 地质矿产部岩溶地质研究所 |
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| 摘 要： | <正> 洞穴溶蚀形态是指由地下水或洞穴水流的溶蚀(混合溶蚀)和侵蚀作用在洞穴周壁上形成并遗留下来的痕迹,如各种流痕、坑穴、沟槽和突出物等。也叫洞穴微地貌,次生洞穴结构或洞穴小形态。国外常用的术语是Speleogen。 洞穴溶蚀形态是洞穴形态学的重要组成部分。它与洞穴大形态(指洞穴通道本身及其横
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| 关 键 词： | 波痕 流痕 波状流 溶蚀形态 桂林地区 灰岩洞穴 窝穴 |
SOLUTIONAL FEATURES OF LIMESTONE CAVES IN GUILIN AREA |
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| Zhu Xuewen.SOLUTIONAL FEATURES OF LIMESTONE CAVES IN GUILIN AREA[J].Carsologica Sinica,1982(2):93-103. |
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| Authors: | Zhu Xuewen |
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| Institution: | Institute of Karst Geology; Ministry of Geology and Mineral Resources |
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| Abstract: | In this paper the speleogens of limestone caves in the famous Guilin karst peak-forest area are discussed, and a classification proposed. The solutional patterns in the caves can be divided according to their morphologic characteristics into five basic types: orientational flow mark type, pocket type,trough and groove type,tubing type, and cave-wall protruding type. 37 terms of different features are listed. Preliminary study are made on their morphologic characteristics, distribution regularities, genesis,... |
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