Mineralogical, petrographic, and geochemical analyzes which confirm the hydrothermal origin of the sediments that overlie the peridotites of Cerro Matoso, Colombia
The Cerro Matoso deposit, one of the largest open-pit ferronickel mines in the world is formed by a sedimentary succession on top of an abducted ultramafic body that makes part of the Cauca ophiolite complex. The set of rocks was accreted in northwestern Colombia during the Cretaceous and exposed to...
Wedi'i Gadw mewn:
| Cyhoeddwyd yn: | Boletín de Geología |
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| Prif Awduron: | , , , |
| Fformat: | Artigo |
| Iaith: | Inglês |
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Universidad Industrial de Santander
2023
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| Mynediad Ar-lein: | https://www.redalyc.org/articulo.oa?id=349675365004 https://www.redalyc.org/journal/3496/349675365004/ https://www.redalyc.org/journal/3496/349675365004/html/ https://www.redalyc.org/journal/3496/349675365004/349675365004.epub https://www.redalyc.org/journal/3496/349675365004/movil |
| Tagiau: |
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