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Record W2370397690

Breakup of China-Korea Platform and Establishment of North China and Huatai Cratons

2012· article· en· W2370397690 on OpenAlexaboutno aff
Quan Wang

Bibliographic record

VenueActa Geological Sinica · 2012
Typearticle
Languageen
FieldEconomics, Econometrics and Finance
TopicGeochemistry and Geochronology of Asian Mineral Deposits
Canadian institutionsnot available
Fundersnot available
KeywordsCratonGeologyChinaSupercontinentRiftEarth scienceGeochemistryOrogenyPaleontologyTectonicsGeographyArchaeology
DOInot available

Abstract

fetched live from OpenAlex

Half a century ago, the well-known pre-Cambrian crystalline basement outcrops extensively in the southern Northeast China, North China and Alashan Desert of Northwest China, which were considered by T.K. Huang and J.S. Ren as a unitary China-Korea Platform. This idea has been being in use until now. Recently, the studies of tectonostratigraphic terrain demonstrate that the China-Korea Platform is composed of both the North China Craton and the Huatai Craton, and contains 11 terrains in all. The range of North China Craton redefined was limited within northern and western Liaoning province, Hebei province, main part of Shanxi province, and northern Shaanxi province. The other regions of original China-Korea Platform, including southern Jilin province, Liaodong peninsula, Shandong province, northern parts of Anhui and Jiangsu provinces, Henan province, the Shaanxi plain and the Alashan Desert-Helan Mts. constitute the new established Huatai craton. The boundary between two cratons and adjacent Paleozoic organic belts are separated by a series of large faults. The North China Craton is the initial continent crust in whole China, which is composed of 4 terrains, including the Yanliao continent block, Jinji orogenic belt, Mengshan continent block and the Yinshan rift belt. The North China Craton originated from the late Paleoproterozoic (1850Ma) orogeny and collision, which resulted in assembly of the former 3 terrains and finally solidification of the craton. The Yinshan rift belt occurred in Mesoproterozoic and was the remains of separation of North China Craton and Siberia Platform. The prominent features of North China Craton are the unconformity between Paleoproterozoic Hutuo Group and Mesoproterozoic Changcheng System, and the deposition of Mesoproterozoic caprock represented by the Jixian profile. According to these characteristics, only Siberia Platform and Canada Shield in the world are comparable to this craton. Over the crystalline basement of Huatai Craton, the first unconformity between Palaeo-Meso Proterozoic Liaohe Group and Neoproterozoic Xihe Group marked its solidification in about 1000 Ma. Therefore, the origin of Huatai Craton can be traced in the world. It is quite evident that Rodinia was a united ancient continent in Neoproterozoic. In view of Cambrian stratigraphic studies in China, it is believed that the assembly between North China Craton and Huatai Craton occurred at the beginning of the Middle Cambrian (about 536 Ma). Before Middle Cambrian, two cratons belonged to different ancient continents and had never been jointed. Therefore there was no united China-Korea Platform during the period from Archean to early stage of Cambrian.

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 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 score0.020
Threshold uncertainty score0.543

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 head0.018
GPT teacher head0.207
Teacher spread0.189 · 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 teacher head, not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designObservational
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

Citations1
Published2012
Admission routes1
Has abstractyes

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