Geomathematical characterisation of the mineralization indicators: a case study from Tincova magmatic intrusion (Romania)
Indicators of the hydrothermal mineralization in the Tincova Laramian intrusion were tested at the contact zone between the intrusive body and the metamorphic host rocks. The mineralization consists of Cu, Pb and Zn sulfides, arsenopyrite, pyrrhotite and pyrite in gangue of quartz, carbonates, felds...
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| Format: | Article |
| Language: | English |
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Cluj University Press
2011-10-01
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| Series: | Studia Universitatis Babes-Bolyai: Geologia |
| Online Access: | http://scholarcommons.usf.edu/geologia/vol56/iss2/art2/ |