Demonstration of Alpine Structural Phenomena at the Structure of Magnesite Deposit Jelšava - Dúbrava Massif
Magnesite deposits in the Central Western Carpathians belong among the biggest deposits in the Europe. Their today’s structure is mainly the result of the Alpine orogenesis. During this period several deformation stages were active, which deformed the deposit body. This resulted in today’s complicat...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
Croatian Metallurgical Society
2007-01-01
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| Series: | Metalurgija |
| Subjects: | |
| Online Access: | http://public.carnet.hr/metalurg/Metalurgija/2007_vol_46/No_2/MET_46_2_117_122_Sasvari.pdf |