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Record W2323378610 · doi:10.3749/canmin.48.5.1237

HYPOGENE Ba-RICH TODOROKITE AND ASSOCIATED NANOMETRIC NATIVE SILVER IN THE SAN MIGUEL TENANGO MINING AREA, ZACATLAN, PUEBLA, MEXICO

2010· article· en· W2323378610 on OpenAlexvenueno aff
J. Arturo Gómez-Caballero, María Guadalupe Villaseñor-Cabral, Patricia Santiago‐Jacinto, F. Ponce-Abad

Bibliographic record

VenueThe Canadian Mineralogist · 2010
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeochemistry and Elemental Analysis
Canadian institutionsnot available
Fundersnot available
KeywordsGeologyGeochemistryHypogenePyriteAluniteMineralization (soil science)BrecciaCassiteriteZirconVolcanic beltVolcanoMineralogyHydrothermal circulationVolcanic rockSphaleritePaleontologyChemistry

Abstract

fetched live from OpenAlex

The San Miguel Tenango area, in the northern part of the State of Puebla, Mexico, is an old, now-abandoned silver mining district worked intermittently since Colonial times until the 1970s. Ores were high in grade, but had a low metallurgical recovery. We characterize the main ore mineral of this mining area, a Ba-rich manganese oxide with associated native silver, to investigate the cause of the low recovery. The ore deposits of this area consist of veins in Mesozoic limestone and shale, and hydrothermal breccias in early Pliocene dacitic volcanic rocks. Because of the present inaccessibility of the mine workings, only one vein was available for sampling. The ore mineral is Ba-rich todorokite with associated native silver, both occurring as cavity fillings. The vein-type ore deposits are related to adjacent early Pliocene dacitic volcanic rocks consisting of ash-fall tuffs, ash flows, volcanic necks, and a volcanic dome. Transmitted- and reflected-light petrography show that todorokite precipitated during the first stage of mineralization in a wide variety of habits. A second stage of mineralization consists of botryoidal to massive oxides and hydroxides of iron, ending with specular hematite. Filling open spaces in minerals of the second stage are minerals of a third stage consisting of irregular masses of pyrite, chalcopyrite, and pentlandite a few μm across. On the basis of this stage, a hypogene origin is assumed for the previous two stages. An XRD analysis of the vein material revealed the presence of todorokite and an amorphous phase, and probably also a hydrous manganese oxide. Semiquantitative analysis made with SEM–EDS and quantitative analysis with EPMA–SEM showed that the cations in both Mn oxide phases are Ag, Mn, Ba, Ca, Zn, K, Na, Mg, Fe, and Cu, with lesser amounts of Ni, Co, Sb, and Au, the absence of Pb being noteworthy. A TEM study corroborates the presence of todorokite and of an amorphous phase of hydrous manganese oxide, and shows a nanometric crystalline phase that corresponds to manganosite. Also, TEM analyses show that Ag occurs as nanometric particles of native silver adsorbed on the external surfaces of todorokite (not in the tunnels of its structure) and of the amorphous phase. In addition, IR analysis confirms the presence of todorokite. We attribute the low recovery of silver to scavenging of the dissolved silver by todorokite during the metallurgical process.

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)0.000
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: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.421
Threshold uncertainty score0.999

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
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 head0.016
GPT teacher head0.199
Teacher spread0.183 · 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 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

Citations23
Published2010
Admission routes1
Has abstractyes

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