Calcite deformation twins in Pohorje marbles
Marbles in Pohorje occur in lenses and smaller bodies in the southern and southeastern part of the massif. Marbles are very pure, predominantly calcitic and rarely calcitic-dolomitic, containing a maximum of 5 % of non-carbonate mineral phases. The latter comprise pyroxenes (diopside), amphiboles...
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| Главные авторы: | , , |
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| Формат: | Artigo |
| Язык: | Inglês |
| Опубликовано: |
Geological Survey of Slovenia
2018-11-01
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| Серии: | Geologija |
| Предметы: | |
| Online-ссылка: | http://www.geologija-revija.si/dokument.aspx?id=1332 |
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