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Record W7132951508

Experimental and fluid inclusion constraints on the ore metal content and origin of volatiles associated with large NI-CU--PGE deposits

2006· dissertation· W7132951508 on OpenAlexaboutno aff
Jacob James Hanley

Bibliographic record

VenueTSpace · 2006
Typedissertation
Language
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsnot available
Fundersnot available
KeywordsBrineFluid inclusionsMetalBase metalOxidizing agentInclusion (mineral)Partition coefficientSalinity
DOInot available

Abstract

fetched live from OpenAlex

Microanalyses of synthetic fluid inclusions containing a S-free, NaCl brine (20-70 wt% eq. NaCl) that was reacted with silicate melt and Pt and Au metal at T=600-800°C, P=1.5 kbar show that both metals are significantly soluble (Cfluidmetal 1-103 ppm) at moderately oxidizing (Ni-NiO) conditions, and partition strongly into the fluid phase (Dfluid/meltmetal = 102-103). Maximum dissolved Pt and Au concentrations decrease by sim;2 log units with increasing salinity from 20 to 70 wt% eq. NaCl. Maximum dissolved Au concentrations increase approximately sim;1 log unit for every 100°C increase in brine temperature. The negative correlation between trapped metal concentration and salinity may be the result of the "salting-out" of neutral metal complexes [e.g., aqueous PtCl3H or Pt(OH)2-(H2On) as the NaCl0 content increases in the fluid and free H2O is consumed. Due most likely to slow metal-fluid-melt equilibrium, microanalysis of fluids trapped using synthetic fluid inclusion methods allows only semi-quantitative estimation of minimum (non-equilibrium) precious metal solubility. Microanalyses of fluid inclusions from the footwall Cu-Ni-PGE systems at Sudbury, Canada, and pegmatites and cumulate rocks below the J-M reef in the Stillwater Complex, U.S.A. show that Na-Ca-K-Fe-Mn-Ba-Pb-Sr-Zn-rich brines ( sim;30-80 wt% eq. NaCl) and non-aqueous volatiles (CH4 vapour; liquid/supercritical CO2; halide melt) carried ppm concentrations of precious/accessory metals (Pt, Pd, Au, Ag, Sn, Ag, Bi) and up to wt% concentrations of base metals (Cu) at the time of their entrapment. Volatile P-T-X characteristics show major similarities at Sudbury and Stillwater, notably evidence for carbonic fluid-brine immiscibility and the selective partitioning of ore metals into the carbonic fluid phase. Inclusion assemblages record a prolonged evolution of volatiles. At near-solidus conditions, inclusions trapped C and Cl-rich volatiles that exsolved from and coexisted with a high Cl/H2O residual silicate liquid or fractionated sulfide liquid at sim;700-800°C. At post-cumulus conditions, inclusions trapped hybrid fluid compositions derived by the interaction of magmatic brines with crystalline wall-rocks, sulfides, or groundwater, and later modified by carbonic fluid-brine immiscibility and metal reprecipitation. Ore metals in the volatiles were derived through interaction with PGE-bearing sulfide assemblages or possibly by the partitioning of ore metals from sulfide liquid.

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)0.001
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Bench or experimental · Consensus signal: Bench or experimental
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.005
Threshold uncertainty score0.009

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.001
Scholarly communication0.0000.000
Open science0.0000.001
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 head0.021
GPT teacher head0.248
Teacher spread0.227 · 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 designBench or experimental
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
Published2006
Admission routes1
Has abstractyes

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