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Record W2347262480

Rheology and dynamics of Qinling orogenic belt and its grade-separation-style structure

2005· article· en· W2347262480 on OpenAlex

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.

aboutThe title or abstract carries a Canadian signal from the geographic lexicon.
no affNo Canadian affiliation: this work is invisible to an affiliation-only frame.
No Canadian affiliation. An affiliation-only frame, the usual design, would never have seen this work. It is one of the works that make the case for inverting the frame.

Bibliographic record

VenueProgress in geophysics · 2005
Typearticle
Languageen
FieldEconomics, Econometrics and Finance
TopicGeochemistry and Geochronology of Asian Mineral Deposits
Canadian institutionsnot available
Fundersnot available
KeywordsGeologyCrustSubductionAsthenosphereMantle (geology)LithosphereGeophysicsMantle convectionOceanic crustMetamorphic core complexSeismologyPetrologyTectonicsExtensional definition
DOInot available

Abstract

fetched live from OpenAlex

The preexistence of Qinling Indosinian Orogenic Belt which widly attracts domestic and oversea geologicians' attentions is a basin-mountain system which formed on the upper crust with most powerful inertial force and is controlled by the E-W strike-slip normal faults and by the process of gravity and latitudinal shear stress derived from gradual variation of the Earth's rotation rate.It is not a channel-arc-basin system formed by subduction.Its orogenic mechanism is that the rigid upper crust's bottom crystalline basement of southern Qinling downcast basin has been subducted under the weak middle crust's plastic layer of northern Qinling rift rising mountain,so it is a intracrust thrust superimposed orogens and not a plate collisional orogenic belt derived from the lithosphere subducting into the asthenosphere.Its power was the meteorite impact which had formed a 100km diameter impact crater before 212 Ma in Ontario,Canadian.It is not mantle convection that drives plates drifting and colliding,but the strong horizontal compression from south to north derived from the Earth's rotation rate sharply slowing down caused by the meteorite impact.Its ultrahigh-pressure metamorphic belt was caused by intracrust subduction dynamical effect and not by continent crust subducting in 100 km-deep-temperature-pressure condition.Its grade-separation-style structure was the result which the anomaly Earth's mantle responsed to the gravity unbalancing caused by new different orientation meso-cenozoic block basins on the upside crust,and not the non-coupling relation between the mantle plume active uplifting and primary W-E orogenic belt.

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: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.211
Threshold uncertainty score0.613

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 head0.009
GPT teacher head0.231
Teacher spread0.221 · 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