MétaCan
Menu
Back to cohort
Record W2378158209

Characteristics of Composition of Metamorphic Fluid in Funiu Tectonic Belt and Its Tectonic Significances

2013· article· en· W2378158209 on OpenAlex
Ren Shenglia

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

affAt least one author lists a Canadian institution in the pinned OpenAlex snapshot.

Bibliographic record

VenueDizhi lunping · 2013
Typearticle
Languageen
FieldEngineering
TopicGeoscience and Mining Technology
Canadian institutionsUniversity of Waterloo
Fundersnot available
KeywordsGeologyGreenschistMetamorphismMetamorphic rockGeochemistrySubductionFluid inclusionsTectonicsQuartzPetrologySeismologyPaleontology
DOInot available

Abstract

fetched live from OpenAlex

The Funiu tectonic belt contains many shear zones in which syntectonic quartz veins are well developed. Mineral component of veins are mainly quartz and there are many fluid inclusions and gas liquid inclusion inclusions in them. The composition of inclusions is characteristic by medium to high salinity,low CO2,low δ18O ~ δD and a small amount of organic matter and with homogenization temperature of 170. 6 ~ 337. 8 ℃and pressure of 0. 27 ~ 0. 87 GPa calculated by muscovite geobarometer. The result shows the metamorphic fluid component and isotopes are inherited from original rocks formed in submarine volcanic eruptions environment. The metamorphism of the Funiushan tectonic belt belongs to greenschist facies and the high pressure suggests the tectonic setting is a subduction zone. The characters of fluid inclusions reflected the Kuanping rock block and the Erlangping rock block subducted beneath the North China Plate in turn and generated strong deformation and weak metamorphism.

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.

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)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation 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 score0.351
Threshold uncertainty score0.362

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
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 head0.011
GPT teacher head0.208
Teacher spread0.196 · 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