| 论贵州岩溶水赋存的地貌规律性 |
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| 引用本文： | 杨明德. 论贵州岩溶水赋存的地貌规律性[J]. 中国岩溶,1982,1(2): 81-91. |
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| 作者姓名： | 杨明德 |
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| 作者单位： | 贵阳师范学院地理系 |
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| 摘 要： | 贵州地处我国南方一个亚热带岩溶化高原,岩溶水丰富、赋存条件复杂,是在地质、地貌、气候三者长期共同作用下演变而成。本文从地貌侧面对岩溶水在上升地貌发育区的一系列表现进行了初步研究,提出了岩溶水的二元结构、三维空间规律、地貌富水面以及地下河系补给类型等新认识;对岩溶水开发利用也作了地貌条件的分析。
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| 关 键 词： | 富水 岩溶水 贵州岩溶 岩溶地貌 向斜 剥夷面 补给型 地下分水岭 浅层岩溶 地下河 |
THE GEOMORPHOLOGICAL REGULARITIES OF KARST WATER OCCURENCES IN GUIZHOU PLATEAU |
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| Yang Mingde. THE GEOMORPHOLOGICAL REGULARITIES OF KARST WATER OCCURENCES IN GUIZHOU PLATEAU[J]. CARSOLOGICA SINICA,1982,1(2): 81-91. |
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| Authors: | Yang Mingde |
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| Affiliation: | Department of Geography; Guiyang Teachers'College |
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| Abstract: | The Guizhou Plateau is situated in the subtropical zone of southwest China.The Plateau has been uplifted strongly since the Quaternary period. Carbonate rocks are widely distributed and karst is well developed,forming typical features over the plateau. The conditions for karst water occurences are very complicated , controlled mainly by the evolution of local geomorphological , geological and climatical environments. The author has investigated the geomorphological regularities of karst wate... |
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