Preliminary Note on the Control of Gold Mineralization in South-West of Burkina Faso (West Africa): The Case of Zone B of the Gnimi-Yabogane Deposit

Analysis of gold mineralization in the Gnimi-Yabogane B zone, in the commune of Dano in southwest Burkina Faso, within the Boromo greenstone belt, reveals local geology comprising volcano-sedimentary rocks, meta-andesite, amphibolitic gabbros, and granodiorites. The study highlighted three phases of deformation (D1, D2, D3), with mineralization mainly controlled by the D2 phase, responsible for the development of NE-SW shear corridors. Deformation markers show that the D1 shear zones are sinistral and the D2 dextral, with gold mainly associated with sulfide-rich brecciated smoky quartz veins. These results confirm structural control of the Mineralization at Area B of the Gnimi-Yabogane deposit in the southwest region.

Authors

Publication Details

Journal
Open Journal of Geology
Published
2025-01-01
DOI
https://doi.org/10.4236/ojg.2025.154009
Primary Topic
Geological and Geochemical Analysis
Type
article
Field-Weighted Citation Impact
0.00
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Preliminary Note on the Control of Gold Mineralization in South-West of Burkina Faso (West Africa): The Case of Zone B of the Gnimi-Yabogane Deposit

Sâga Sawadogo, Abraham Seydoux Traoré, Oussény Sourgou, Rayangniwendé Abdoul Rasaky Kaboré
Open Journal of Geology
Geological and Geochemical Analysis
article

Preliminary Note on the Control of Gold Mineralization in South-West of Burkina Faso (West Africa): The Case of Zone B of the Gnimi-Yabogane Deposit

Sâga Sawadogo, Abraham Seydoux Traoré, Oussény Sourgou, Rayangniwendé Abdoul Rasaky Kaboré
article en

Abstract

Analysis of gold mineralization in the Gnimi-Yabogane B zone, in the commune of Dano in southwest Burkina Faso, within the Boromo greenstone belt, reveals local geology comprising volcano-sedimentary rocks, meta-andesite, amphibolitic gabbros, and granodiorites. The study highlighted three phases of deformation (D1, D2, D3), with mineralization mainly controlled by the D2 phase, responsible for the development of NE-SW shear corridors. Deformation markers show that the D1 shear zones are sinistral and the D2 dextral, with gold mainly associated with sulfide-rich brecciated smoky quartz veins. These results confirm structural control of the Mineralization at Area B of the Gnimi-Yabogane deposit in the southwest region.

Open Journal of GeologyVol. 15(04)
Openalex Percentile: Top 90%
Geological and Geochemical Analysis
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.