The dissolution and conversion of Gypsum and Anhydrite
The development of karst is a complex system driven by the dissolution of a host rock and the subsequent removal of dissolved matter by moving water. It is the process that, at various stages, initiates or triggers associated processes including erosion, collapse and subsidence. The dissolution of s...
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| Format: | Article |
| Language: | English |
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University of South Florida Libraries
1996-01-01
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| Series: | International Journal of Speleology |
| Online Access: | http://ijs.speleo.it/pdf/6.46.25_Klimchouk.pdf |