Mineralogy of Iza Cave (Rodnei Mountains, N. Romania)
The secondary minerals from Iza Cave result from the interactions of karst water and/or cave atmosphere with a variety of sedimentaryand metamorphic rocks. The cave passages expose at various extents Eocene limestones and conglomerates, Oligocene blackshales, Upper Precambrian micaschists, marble an...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
University of South Florida Libraries
2011-07-01
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| Series: | International Journal of Speleology |
| Subjects: | |
| Online Access: | http://scholarcommons.usf.edu/ijs/vol40/iss2/10/ |