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Record W3004047941

The lithosphere of Ellesmere Island and adjacent northwestern Greenland (CALE 'A' transect onshore)

2013· article· en· W3004047941 on OpenAlexaboutno aff
Randell Stephenson, Christian Schiffer, G N Oakey

Bibliographic record

Venuenot available
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological Studies and Exploration
Canadian institutionsnot available
Fundersnot available
KeywordsTransectGeologyLithospherePhysical geographyOceanographyEarth sciencePaleontologyGeographyTectonics
DOInot available

Abstract

fetched live from OpenAlex

Ellesmere Island, in Canada’s Arctic, comprises a series of ~SW-NE trending tectonic provinces, the crustal structure and geological expression of which represent a combination of interplate, accretionary orogenesis in the Palaeozoic (Caledonian equivalent and Ellesmerian orogenies) and intraplate orogenesis in the Cenozoic (Eurekan Orogeny). The present-day topography of Ellesmere Island is closely related to the crustal architecture of these tectonic provinces, which includes the adjacent polar continental margin. A two-dimensional lithosphere-scale model is presented that crosses Ellesmere Island from northern Baffin Bay to the Arctic Ocean, part of Transect “A” of the Circum-Arctic Lithosphere Evolution (CALE) project. The model is based on gravity and magnetic data constrained by mapped geological structure as well as a not yet unpublished Receiver Function study, based on teleseismic data acquired between 2010 and 2012 by a passive seismological array on Ellesmere Island called “ELLITE”. In northern Baffin Bay and on parts of the polar margin of Ellesmere Island (and adjacent northwestern Greenland), published crustal scale seismic refraction velocity models also provide some constraint to the lithosphere model. The most recent tectonic event governing the geological and physiographic character of Ellesmere Island is the Eurekan Orogeny, an intraplate orogeny that developed as a consequence of North Atlantic-Arctic plate reorganisations and the resulting convergence of Greenland against Ellesmere Island in the Palaeogene. The basement of the Eurekan orogen comprises Precambrian-aged lithosphere in its northernmost (Pearya terrane) and southeasternmost (Greenland-Canada craton) parts as well as possibly younger lithosphere accreted during Palaeozoic orogenesis in central Ellesmere Island. Its southern margin, marking the southern terminus of the constructed lithosphere model, comprises the late Precambrian-Early Palaeozoic passive continental margin of Laurentia. The preliminary Receiver Functions show signatures of strong intracrustal velocity discontinuities, possibly indicating major vertical structural differences in in the central part of Ellesmere Island, which are absent in the north and south. The lithosphere model is interpreted in the context of plate convergence processes in the Palaeozoic and large-scale intraplate shortening in the Cenozoic with extensional tectonics dominating throughout the Mesozoic.

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 machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: metacan-v3-hybrid-931329e0061cValidation 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 score0.236
Threshold uncertainty score0.475

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.001
Science and technology studies0.0010.000
Scholarly communication0.0010.000
Open science0.0000.001
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0030.000

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 head0.012
GPT teacher head0.173
Teacher spread0.162 · 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 source (direct Gemma or distilled Codex), 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

Citations0
Published2013
Admission routes1
Has abstractyes

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