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Record W4402518176 · doi:10.26565/2410-7360-2024-60-01

Tectonic Evolution of the Intra-plate Structures of Sarmatia in the Phanerozoic. 1. Geophysical analysis of structural and substance differentiation of the lithosphere and tectonic divisibility of the Earth's crust

2024· article· en· W4402518176 on OpenAlex
Оleksii Bartaschuk, Vasyl Suyarko, Oleksandr Chuienko, Bruce J. Perry

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

VenueVisnyk of V N Karazin Kharkiv National University series Geology Geography Ecology · 2024
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsHudbay Minerals (Canada)
Fundersnot available
KeywordsLithosphereGeologyCrustGeophysicsMantle (geology)TectonicsStructure of the EarthTectonophysicsPlate tectonicsContinental crustCratonPetrologySeismology

Abstract

fetched live from OpenAlex

Purpose. The structure of the Sarmatia`s llithospheric plate was studied based on the latest integrated geological, geophysical, tectonophysics, aerocosmo-geological, neo-tectonic data and the gravity, magnetic, dense and seismic (GSZ, seismotomography) modeling data. The aim of the study to reveal the nature of heterogeneities of the Sarmatia Lithosphere and their influence on the nature of the process of structural and material differentiation of the Earth's continental crust. Method. A comparative geotectonic analysis of the structure, composition, and relationships of individual layers of the consolidated crust, the Moho section, and the sub-crustal mantle was performed. According to the results of the analysis, the nature of the relationship between the structure and composition of the Lithosphere component surfaces and the layers of the Earth's crust, the peculiarities of the tectonic division of the Pre-Rifean craton core of Sarmatia were clarified. Results. The relationship and regularities of the spatial distribution of individual floors of the Lithosphere, the layers of the Earth's continental crust and the core-mantle mixture, the structure of the Moho interface and the sub-crustal mantle on the territory of Ukraine have been clarified. Based on the comparison of the modern segmentation of the consolidated crust with the structure of the lithosphere layers, it was established that the modern structural and material heterogeneity of the Sarmatia plate core is determined by the original, "built-in" anisotropy of the Lithosphere, while the structure of the Earth's crust does not have an unequivocal connection with the relief of the sole of the modern seismic lithosphere. Exceptions are its rise with the formation of mantle dome structures in separate areas of the Western and Eastern micro-plates and under the Lokhvytskyi segment of the Dnipro-Donetsk Avlacogen. Scientific novelty. The nature of the impact of the heterogeneity of the Sarmatia`s lithosphere, "frozen" during the stabilization of the Pre-Rifean craton core of the East European Platform, on the modern segmentation and structural-material differentiation of the Earth's continental crust has been clarified. Scientific novelty. For the first time, a conclusion was made about the deformational nature of the structural differentiation of the continental crust of Sarmatia, which was formed against the background of the initial anisotropy of the Lithosphere under the influence of processes of mantle activation at the stages of tectonic evolution in the Phanerozoic. Practical significance. The obtained data on the geodynamic relationship between the structural surfaces of the lithosphere, the layers of the Earth's crust and the coromantium mixture can be used for geological interpretation when elucidating the geodynamic conditions of the formation and tectonic evolution of the intra-plate geostructures of Sarmatia in the Phanerozoic.

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 score0.023
Threshold uncertainty score0.992

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.002
Science and technology studies0.0000.002
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 head0.004
GPT teacher head0.175
Teacher spread0.171 · 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