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Record W4417328806 · doi:10.1177/25726838251405980

Alteration and lithogeochemical characterisation of the Esaase gold deposit in the Paleoproterozoic Birimian Terrane of Ghana

2025· article· en· W4417328806 on OpenAlexaboutno aff
Boateng Agyenim, Kofi Adomako‐Ansah

Bibliographic record

VenueApplied Earth Science Transactions of the Institutions of Mining and Metallurgy · 2025
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsnot available
FundersSociety of Economic Geologists Foundation
KeywordsPetrographyHydrothermal circulationMetamorphic rockTerranePyriteChalcopyrite

Abstract

fetched live from OpenAlex

The Esaase gold deposit is located in the Asankrangwa gold belt and within the Paleoproterozoic Birimian Supergroup of the Kumasi basin. The deposit represents an important example of a structurally controlled turbidite-hosted gold system. Despite its economic significance, the geochemical processes controlling the element mobility during mineralisation remain poorly understood. This study presents an integrated petrographic and mass balance investigation of the Esaase gold deposit to characterise alteration processes and quantify the elemental mass transfer associated with the hydrothermal mineralisation. Petrographic studies revealed two major stages: (I) metamorphic and (II) hydrothermal. Stage II is associated with gold mineralisation. Metamorphic alteration is characterised by fine-grained sericite, chlorite, paragonite, and albite, while hydrothermal alteration is characterised by coarse-grained sericite, chlorite, carbonates, quartz, albite, paragonite, pyrite, arsenopyrite, and traces of chalcopyrite and gold. (Na 2 O/Al 3 O 2 vs. K 2 O/Al 3 O 2 ) Isocon-based mass balance calculations reveal a net mass gain of 16.67%, with significant enrichment in Au, As, Sb, Bi, Pb, Te, Se, Sb, Cr, Ni, and Cu, and marked depletion in Cao without significant changes in K 2 O and Na 2 O. These geochemical trends reflect localised but efficient fluid-rock interaction along structurally controlled hydrothermal pathways. The alteration assemblages are dominated by sericite-chlorite over sericite-albite, as supported by alkali-alumina molar ratios (Na 2 O/Al 3 O 2 vs. K 2 O/Al 3 O 2 ), consistent with alteration haloes surrounding sheeted quartz-carbonate veins. The deposit geology, alteration mineralogy, and lithogeochemistry of the Esaase turbidite-hosted gold deposit are similar to other world-class turbidite-hosted gold deposits, such as Bendigo in Australia, Meguma in Canada, Reefton in New Zealand, and Shangxu in China. This study establishes the quantitative mass balance assessment of the hydrothermal alteration at Esaase, demonstrating how moderate net mass gains reflect structurally controlled fluid flow and mineralisation. The findings provide new constraints on the genetic interpretations and support targeted exploration strategies in the Kumasi basin and similar geological settings.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.021
Threshold uncertainty score0.042

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.001
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.015
GPT teacher head0.214
Teacher spread0.199 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designObservational
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations0
Published2025
Admission routes1
Has abstractyes

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