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Record W1490421239 · doi:10.1029/2012tc003104

Evolution of the Yiwulushan metamorphic core complex from distributed to localized deformation and its tectonic implications

2012· article· en· W1490421239 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.

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

Bibliographic record

VenueTectonics · 2012
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsWestern University
Fundersnot available
KeywordsGeologyMetamorphic core complexMetamorphic rockTectonicsCore (optical fiber)Deformation (meteorology)SeismologyPaleontologyExtensional definition

Abstract

fetched live from OpenAlex

The Yiwulushan metamorphic core complex (YSMCC) is situated in the northern part of the eastern North China Craton (NCC) that experienced significant lithospheric thinning in an extensional regime during the Late Mesozoic. We present structural and geochronological evidence to show that the YSMCC underwent NNE‐SSW extension in the Late Jurassic and WNW‐ESE extension in the Early Cretaceous. We show that the YSMCC started with a sub‐horizontal shear zone referred to as the Yiwulushan detachment shear zone (YDSZ) in the Late Jurassic between 157 and 147 Ma with a top‐to‐the‐SSW shear sense. The YDSZ was subjected to limited doming probably toward the end of its formation. The NNE‐striking, WNW‐dipping Waziyu normal shear zone (WZYSZ) was formed along the western margin of the core complex during the Early Cretaceous, and truncates the earlier YDSZ. The whole core complex underwent doming in a rolling‐hinge manner in the end of the latest Early Cretaceous. Thereafter, the YSMCC was overprinted by brittle normal faults along its western margin in the Late Cretaceous. Development of the initially flat‐lying YDSZ is associated with diffuse mid‐crustal flow whereas the formation of the rolling‐hinge type WZYSZ is characterized by localized deformation. The Late Jurassic more diffuse deformation has a rather constant top‐to‐the‐SSW shearing and produced a variety of shear‐related structures such as recumbent isoclinal folds and transposition foliation. The YSMCC evolution also demonstrates that the Late Mesozoic extension along the northern part of the eastern NCC started as early as the Late Jurassic rather than the previously proposed Early Cretaceous.

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 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 score0.028
Threshold uncertainty score0.999

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)0.0020.000

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 head0.035
GPT teacher head0.227
Teacher spread0.192 · 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