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A new occurrence of (gold-bearing) graphite in the Assosa region, Benishangul-Gumuz State, W. Ethiopia

A new occurrence of (gold-bearing) graphite in the Assosa region, Benishangul-Gumuz State, W. Ethiopia
A new occurrence of (gold-bearing) graphite in the Assosa region, Benishangul-Gumuz State, W. Ethiopia
The Assosa region of western Ethiopia hosts newly discovered and potentially highly economic graphite-bearing schist units. Due to its unique physical and chemical properties, graphite is quickly becoming an increasingly important economic resource. Graphite occurs over much of the area, and is hosted predominantly by quartz-graphitic schist, quartz-feldspar-mica schist and quartzite. The quartz-graphitic schist covers an area of 37 km2, forming steep valleys and ridges across a 190 km long belt. Graphite is texturally-variable within and across units. Crystal habit varies from highly crystalline to irregular flakes. Flake sizes range from amorphous and crystalline small flake to coarse large flake (> 150 μm), with beneficiation of ~ 70% and yield potential of > 95% (froth flotation methods). The license area is already a well-known gold-hosting area, and potentially economic gold deposits occur within the graphite-bearing units. Overall, the site shows excellent geochemical indicators, field observations and historical accounts of high gold content. It is suggested that textural variations may be the product of (1) early in-situ formation during (early- to late-Proterozoic) prograde metamorphism and (2) later vein-type mineralization during retrograde metamorphism. The discovery of graphite in western Ethiopia is the first documented and preliminary studies suggest a high economic potential for the deposits.
2159-581X
417-435
Bullock, Liam
c6ffb9b0-0a54-4ab2-9edb-f97280e6ce2d
Owen J. Morgan,
0565aecd-a4c1-45a3-b26c-ee64c1224750
Bullock, Liam
c6ffb9b0-0a54-4ab2-9edb-f97280e6ce2d
Owen J. Morgan,
0565aecd-a4c1-45a3-b26c-ee64c1224750

Bullock, Liam and Owen J. Morgan, (2015) A new occurrence of (gold-bearing) graphite in the Assosa region, Benishangul-Gumuz State, W. Ethiopia. Journal of Earth Science and Engineering, 5 (7), 417-435. (doi:10.17265/2159-581X/2015.07).

Record type: Article

Abstract

The Assosa region of western Ethiopia hosts newly discovered and potentially highly economic graphite-bearing schist units. Due to its unique physical and chemical properties, graphite is quickly becoming an increasingly important economic resource. Graphite occurs over much of the area, and is hosted predominantly by quartz-graphitic schist, quartz-feldspar-mica schist and quartzite. The quartz-graphitic schist covers an area of 37 km2, forming steep valleys and ridges across a 190 km long belt. Graphite is texturally-variable within and across units. Crystal habit varies from highly crystalline to irregular flakes. Flake sizes range from amorphous and crystalline small flake to coarse large flake (> 150 μm), with beneficiation of ~ 70% and yield potential of > 95% (froth flotation methods). The license area is already a well-known gold-hosting area, and potentially economic gold deposits occur within the graphite-bearing units. Overall, the site shows excellent geochemical indicators, field observations and historical accounts of high gold content. It is suggested that textural variations may be the product of (1) early in-situ formation during (early- to late-Proterozoic) prograde metamorphism and (2) later vein-type mineralization during retrograde metamorphism. The discovery of graphite in western Ethiopia is the first documented and preliminary studies suggest a high economic potential for the deposits.

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Published date: 28 July 2015

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Local EPrints ID: 421649
URI: https://eprints.soton.ac.uk/id/eprint/421649
ISSN: 2159-581X
PURE UUID: ded84a77-d0ee-4ee0-bca7-82d2ed2692eb

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Date deposited: 19 Jun 2018 16:30
Last modified: 13 Mar 2019 18:24

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