Lateritization and enrichment of ferruginous protore during the peneplanation between uplifts – the case of Mekaneselam iron deposit, NW Ethiopian plateau
Mekaneselam iron deposit is located in the NW Ethiopian Plateau. The area is constituted by limestone at the bottom followed by mudstone, sandstone and basalt at the top. Geological mapping, geochemical, mineralogical and stratigraphic investigations were conducted to explain the genesis of the depo...
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| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Taylor & Francis Group
2024-11-01
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| Series: | Geology, Ecology, and Landscapes |
| Subjects: | |
| Online Access: | https://www.tandfonline.com/doi/10.1080/24749508.2024.2429207 |
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