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Compressional salt tectonics and synkinematic strata of the western <scp>K</scp>uqa foreland basin, southern <scp>T</scp>ian <scp>S</scp>han, <scp>C</scp>hina

2012· article· en· W2109716983 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

VenueBasin Research · 2012
Typearticle
Languageen
FieldEarth and Planetary Sciences
Topicearthquake and tectonic studies
Canadian institutionsnot available
FundersPetroChina Company Limited
KeywordsDiapirGeologyForeland basinSalt tectonicsStructural basinSedimentary depositional environmentGeochemistryTectonicsCanada BasinAnticlinePaleontologyGeomorphology

Abstract

fetched live from OpenAlex

Abstract The synkinematic strata of the K uqa foreland basin record a rich history of C enozoic reactivation of the P alaeozoic T ian S han mountain belt. Here, we present new constraints on the history of deformation in the southern T ian S han, based on an analysis of interactions between tectonics and sedimentation in the western K uqa basin. We constructed six balanced cross‐sections of the basin, integrating surface geology, well data and a grid of seismic reflection profiles. These profiles show that the Q iulitage fold belt on the southern edge of the K uqa basin developed by thin‐skinned compression salt tectonics. The structural styles have been influenced by two major factors: the nature of early‐formed diapirs and the basinward depositional limit of the K umugeliemu salt. Several early diapirs developed in the western K uqa basin, soon after salt deposition, which acted to localize the subsequent shortening. Where diapirs had low relief and a thick overburden they tended to tighten into salt domes 3000–7000 m in height. Conversely, where the original diapirs had higher relief and a thinner overburden they tended to evolve into salt nappes, with the northern flanks of the diapirs thrusting over their southern flanks. Salt was expelled forward, up dip along the mother salt layer, tended to accumulate at the distal pinch‐out of K umugeliemu salt located at the Q iulitage fold belt. Furthermore, the synkinematic strata (6–8 km thick) of the K uqa basin indicate that during the C enozoic reactivation of the T ian S han, shortening of the western K uqa basin was mainly in the hinterland until the early M iocene. Then, compression spread simultaneously southwards to the D awanqi anticline, the Q iulitage fold belt and the southernmost blind detachment fold at the end of M iocene. The western K uqa basin has a shortening of ca . 23 km. We consider that ca . 9 km was consumed from the end of the M iocene (5.2/5.8 Ma) to the early P leistocene (2.58 Ma) and another ca . 14 km have been absorbed since then. Thus, we obtain a ca . 3.4/2.8 mm year −1 average shortening from 5.2/5.8 to 2.58 Ma, followed by a 60–90% increase in average shortening rate to ca . 5.4 mm year −1 since 2.58 Ma. This suggests that the reactivation of the modern T ian S han has been accelerating up to the present day.

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)0.005
metaresearch head score (Gemma)0.008
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesMeta-epidemiology (narrow), Science and technology studies, Insufficient 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 score0.064
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0050.008
Meta-epidemiology (narrow)0.0010.001
Meta-epidemiology (broad)0.0010.000
Bibliometrics0.0010.001
Science and technology studies0.0020.002
Scholarly communication0.0010.001
Open science0.0020.001
Research integrity0.0010.002
Insufficient payload (model declined to judge)0.0000.001

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 head0.052
GPT teacher head0.293
Teacher spread0.240 · 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