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Record W1989991224 · doi:10.4043/23795-ms

Developing Geophysical Constraints on the History of the Amerasian Basin of the Arctic Ocean

2012· article· en· W1989991224 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

VenueOTC Arctic Technology Conference · 2012
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological Studies and Exploration
Canadian institutionsnot available
Fundersnot available
KeywordsGeologyUnconformityPaleontologyRiftSeafloor spreadingBasementStructural basinCenozoicSeismic refractionStratigraphyGeophysicsSeismologyTectonics

Abstract

fetched live from OpenAlex

Abstract The Chukchi Edges project was designed to establish the relationship betweenthe Chukchi Shelf and Borderland and indirectly test theories of opening forthe Canada Basin. During this cruise, ~5300 km of 2D multi-channel seismicprofiles and other geophysical measurements (swath bathymetry, gravity, magnetics, sonobuoy refraction seismic) were collected from the RV Marcus G. Langseth across the transition between the Chukchi Shelf and ChukchiBorderland. These profiles reveal extended basins separated by faulted high-standingblocks. Basin stratigraphy can be subdivided on the basis of gross stratalgeometry, reflection terminations and inferred unconformities. The wedge-shapedsynrift sequences terminate against the basement highs and/or major faults, burying the basement topography. The inferred postrift seismic units are morenearly tabular, but thicken locally due to compaction of underlying synriftsediments. Reflection character is dominated by alternating high and low amplitudecontinuous reflectors which may be consistent with pelagic or turbiditesediments. Chaotic units are also observed, which may indicate mass-flowdeposits. The truncated sediments over the basement highs of the Chukchi Shelf, Chukchi Plateau and Northwind Ridge suggest major erosion due both to glacialplanation and earlier erosional events perhaps associated with basement upliftprior to or during rifting and extension. It is believed that the bulk of the synrift sediments are Mesozoic in age. Certainly Cenozoic sediments are also preserved in these basins, but theposition of the boundary is uncertain. Locally, continuous reflectors areobserved underlying the rift basin fill. These older units, of very uncertainage, would, if sampled, provide constraint on the history and affinities of theChukchi Borderland. In addition to the extensional basins, a number of small symmetric basinsare observed on the flanks of the Chukchi Plateau. These basins may betranstensional and argue for a 2nd phase of tectonism, which overprinted theobvious extensional fabric of the Borderland. This is supported by theobservation of uplifted postrift sediments on the flanks of some of theintermedial basement highs. Understanding the timing, distribution and extentof these two phases of tectonism, relative to the known history of N-Sextension on the Chukchi shelf and the apparent orthogonal extension observedon the Beaufort Shelf will further constrain the unknown history of the CanadaBasin.

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 score0.101
Threshold uncertainty score0.715

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 studies0.0000.002
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

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 head0.038
GPT teacher head0.203
Teacher spread0.165 · 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