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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Bibliographic Details
Main Authors: Belayneh Digafe, Worash Getaneh, Balemwal Atnafu
Format: Article
Language:English
Published: Taylor & Francis Group 2024-11-01
Series:Geology, Ecology, and Landscapes
Subjects:
Online Access:https://www.tandfonline.com/doi/10.1080/24749508.2024.2429207
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