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Record W4406053654 · doi:10.1016/j.gca.2024.12.027

The chemical and isotopic characterization of the pyrite to pyrrhotite desulfidation reaction across the metamorphic gradient of a metasedimentary basin

2025· article· en· W4406053654 on OpenAlexaff
Bruna Coldebella, Crystal LaFlamme, Isaac S. Malta, Carl Guilmette, Guillaume Barré, Georges Beaudoin, Laure Martin, Dany Savard

Bibliographic record

VenueGeochimica et Cosmochimica Acta · 2025
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsUniversité du Québec à ChicoutimiUniversité Laval
Fundersnot available
KeywordsPyrrhotiteMetamorphic rockPyriteGeologyGeochemistryCharacterization (materials science)MineralogyMaterials scienceNanotechnology

Abstract

fetched live from OpenAlex

During prograde metamorphism, sulfur is released through the pyrite to pyrrhotite desulfidation reaction. This process is believed to supply sulfur and metals to metamorphic fluids, potentially contributing to the formation of orogenic gold deposits. A deeper understanding of this reaction can therefore help unravel the mobility of sulfur, gold and other metals in metamorphic fluids during prograde metamorphism. We present a novel in situ study of multiple sulfur isotopes combined with trace elements, focused on the texturally-constrained pyrite to pyrrhotite desulfidation reaction. This reaction is documented in detail along a prograde, Barrovian metamorphic field gradient − increasing from the biotite through the garnet, staurolite, and sillimanite zones − recorded in the Pontiac Group metasedimentary sequence, which is fault-bound to the southern Abitibi Subprovince and its orogenic gold deposits. The prograde pyrite to pyrrhotite reaction texture, where pyrrhotite (Po) replaces corroded pyrite (Py1), is identified in rocks from the biotite and garnet metamorphic zones. Py1 and Po coexist in the staurolite zone without a clear textural relationship, and past the sillimanite isograd, Py1 is completely absent with Po in abundance. Py1 and/or Po are replaced by euhedral to subhedral, inclusion-free, late/retrograde pyrite (Py2) in all metamorphic zones. In situ trace element analysis of the sulfide assemblage reveals a decrease, with increasing metamorphic grade, in metal contents such as Au, Ag, Te, Bi, and Se, associated with the prograde replacement of Py1 by Po. Arsenic and Co are preserved and enriched in Py2, while Ni is concentrated in Po, and Cu is redistributed to chalcopyrite. In situ, multiple sulfur isotope analyses show no analytically distinguishable fractionation (δ34S shift of −0.1‰ ± 0.9 and a Δ33S shift of +0.06‰ ± 0.17) between Py1 and Po. These results indicate that the H2S produced by the desulfidation reaction retains the δ34S-Δ33S signature of Py1 across the biotite, garnet, and staurolite zones. This detailed examination of the textural and chemical evolution of sulfides highlights the role of desulfidation in metal mobility. The pyrite to pyrrhotite reaction can be an efficient mechanism for supplying sulfur, Au, Ag, Te, Bi and Se, and if synchronous with the release of fluids and deformation, mobilizing Au through the Earth's crust.

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: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.004
Threshold uncertainty score0.009

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0000.000

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 head0.008
GPT teacher head0.218
Teacher spread0.210 · 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

Citations6
Published2025
Admission routes1
Has abstractyes

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