Travertines and calcareous tufa deposits: an insight into diagenesis
Travertines and calcareous tufa are porous deposits formed by interactions between ambient precipitation of calcium carbonate and resident organisms under different temperature regimes. The distinctions between travertine as thermal spring deposits and calcareous tufa (Kalktuff) as deposits in the s...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Croatian Geological Survey
2008-12-01
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| Series: | Geologia Croatica |
| Subjects: | |
| Online Access: | http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/37 |