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Record W2015018239 · doi:10.2343/geochemj.36.197

High 3He/4He ratios in the Wangu gold deposit, Hunan province, China: Implications for mantle fluids along the Tanlu deep fault zone.

2002· article· en· W2015018239 on OpenAlexaff
Jingwen Mao, Robert Kerrich, Hongyan Li, Yanhe Li

Bibliographic record

VenueGEOCHEMICAL JOURNAL · 2002
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsUniversity of Saskatchewan
FundersNational Natural Science Foundation of China
KeywordsGeologyAsthenosphereMantle (geology)Meteoric waterGeochemistryLithosphereFluid inclusionsShear zoneSedimentary rockFault (geology)QuartzTectonicsSeismologyHydrothermal circulationPaleontology

Abstract

fetched live from OpenAlex

The Wangu shear zone hosting gold deposit is located on splay faults of the regional scale Tanlu deep fault zone that extends to the MOHO and likely through the lithosphere.Fluid inclusions in pyrite from gold bearing veins have 3 He/ 4 He (R/Ra) values of 3.5 to 9.8.Fluid inclusions in pyrite from barren vein have R/Ra values of 0.8, and 0.9.The projections of the analyses in 3 He/ 4 He vs. 40 Ar/ 36 Ar diagram can be separated obviously as two groups and display the variable degrees of mixing between mantle and crustal fluids.Fluid inclusion in quartz from auriferous veins are characterized by a higher temperature (Th = 207 to 310°C), dilute, aqueous carbonic fluids, with δD and δ 18 O values overlapping the magmatic fluids, whereas barren veins have low temperature (Th = 138, 145°C), more saline, aqueous fluid with relatively low, light δD and δ 18 O values, consistent with evolved meteoric water.Lithosphere extension accompanied with displacement of the Tanlu sinistral fault, with development of gas and oil-bearing sedimentary basins proximal to the fault.The CO 2 -bearing fluids have high He contents of up to 0.1% He, 3 He/ 4 He = (3~7.2)R/Ra,40 Ar/ 36 Ar = 573~7744, and δ 13 C CO 2 = -3.4 to -16.9‰ (Xu et al., 1995;Tao et al., 1996).During the lithosphere extension and decompressional melting of asthenosphere, noble gases and CO 2 exsolved from basalt melts, advected up to the Tanlu fault zone into splay faults where gold mineralization developed, and through sedimentary basin.There was mixing with isotopically and compositionally evolved meteoric water.mineralization, based on helium isotope studies (Simmons et al., 1987;Stuart et al., 1995;Hu et al., 1998;Burnard et al., 1999).All of the 3 He/ 4 He ratios in these deposits are between two end members, implying variable degrees of mixing between mantle and crustal fluids.To further address possible contributions of mantle fluids to gold metallogenesis, we have conducted a study of He and Ar isotopes and fluid inclusions in the Wangu gold deposit, Hunan province, China.This is one of several gold deposits distributed along the Tanlu deep fault system.High concentrations of mantle-derived helium and CO 2 have been reported in natural gases from several basins along the Tanlu fault zone (Xu et al., 1995;

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 score0.155
Threshold uncertainty score0.308

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.002
Science and technology studies0.0010.001
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 head0.012
GPT teacher head0.200
Teacher spread0.188 · 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

Citations62
Published2002
Admission routes1
Has abstractyes

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