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Record W4399298948 · doi:10.1080/00206814.2024.2361263

A review of the main tectonic settings of Neoarchaean ore deposits and mineral occurrences in the northern São Francisco Craton, NE Brazil

2024· review· en· W4399298948 on OpenAlexfundno aff
Rafael Gordilho Barbosa, Johildo Salomão Figueirêdo Barbosa, Felipe Padilha Leitzke, Ângela Beatriz de Menezes Leal, Ísis de Moraes Cortez, Rejane Lima Luciano, Basílio Elesbão da Cruz Filho, Jocilene dos Santos Santana, Antônio Marcos Vitória de Moraes

Bibliographic record

VenueInternational Geology Review · 2024
Typereview
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsnot available
FundersConselho Nacional de Desenvolvimento Científico e TecnológicoCoordenação de Aperfeiçoamento de Pessoal de Nível SuperiorSociety of Economic Geologists Canada Foundation
KeywordsGeologyGeochemistryMaficCratonGabbroOceanic crustGreenstone beltBanded iron formationSedimentary rockBasaltArcheanTectonicsPaleontologySubduction

Abstract

fetched live from OpenAlex

In this paper, a compilation of the main Neoarchaean ore deposits, and their tectonic settings, in the northern São Francisco Craton, NE Brazil is presented. The Serrinha and Gavião blocks split up in the Neoarchaean, giving rise to juvenile rocks and metavolcanic-sedimentary sequences within the so-called Mundo Novo-Caraíba-Ibicuí sea. The rocks from the southern Gavião Block served as basement for the Contendas-Mirante sequence, where the Jacaré River Vanadium mine is situated in a stratified gabbro-anorthosite mafic sill, which intruded a Neoarchaean shear zone. On the northern part of the Gavião Block, where oceanic crust was identified by the presence of the Mundo Novo greenstone belt, hydrothermal mineralizations of both lead and zinc were mapped in calc-silicate rocks, which are associated to metamorphosed tholeiitic seafloor basalts and these metabasalts are tectonically intercalated with metadacites. In the Jequié Block, occurs the Ibicuí-Iguaí Iron District, which lies in the suture zone between this tectonic unit and the Itabuna-Salvador-Curaçá belt. These are rocks comprising a sequence of metabasalts and metavolcanic tuff, metakomatiites, kinzigites, quartzites and itabirites. In this belt also occurs the southern Bahia manganese district, where the mineralization is hosted in granulitized metavolcanic-sedimentary sequences. The ore protoliths are chemical sediments composed of spessartite, pyroxmangite, rhodonite, rhodochrosite, magnetite, mesoperthite and quartz. The reducing characteristics of the primary environment are confirmed by the presence of graphite and manganese sulphide (alabandite). This mineralogy produced through supergenic processes, ores with great reserves of pyrolusite and psilomelane. In the northern part of the Itabuna-Salvador-Curaçá Belt, an island arc was identified, where mafic-ultramafic bodies (2580 Ma) intruded at its base, giving rise to the Curaçá-Caraíba Valley Cupriferous District. These bornite and chalcopyrite-rich bodies were generated from a calc-alkaline magma that originated multiple Cu-rich gabbroic and pyroxenitic intrusions.

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 distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.001
metaresearch head score (Gemma)0.001
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesInsufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Other design · Consensus signal: none
GenreCandidate signal: Review · Consensus signal: Review
Teacher disagreement score0.841
Threshold uncertainty score0.999

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0020.001
Bibliometrics0.0000.001
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0010.000
Research integrity0.0000.001
Insufficient payload (model declined to judge)0.0020.000

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 head0.018
GPT teacher head0.285
Teacher spread0.267 · 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 teacher head, not a consensus.

Study designOther design
Domainnot available
GenreReview

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
Published2024
Admission routes1
Has abstractyes

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