Sulphate rocks as an arena for karst development
The rocks in which karst systems develop are most commonly composed of carbonate sulphate and chloride minerals. The sulphate minerals are quite numerous, but only gypsum and anhydrite form extensive masses in sedimentary sequences. Other minerals, which represent sulphates of K, Mg and Na, normally...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
University of South Florida Libraries
1996-01-01
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| Series: | International Journal of Speleology |
| Online Access: | http://ijs.speleo.it/pdf/6.45.25_Klimchouk.Andrejchouk.pdf |