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Record W2282044784 · doi:10.7282/t37943c2

The influence of basin architecture and synrift salt on structural evolution during and after rifting

2013· article· en· W2282044784 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

VenueRutgers University Community Repository (Rutgers University) · 2013
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological formations and processes
Canadian institutionsnot available
Fundersnot available
KeywordsNova scotiaRiftStructural basinGeologySubmarine pipelineArchitecturePaleontologyArchaeologyOceanographyGeography

Abstract

fetched live from OpenAlex

The Orpheus rift basin is part of the eastern North American rift system that formed prior to the opening of Atlantic Ocean. Using 2D seismic-reflection and well data and with information from the adjacent Fundy rift basin, I have defined the styles of deformation that formed during the development of the Orpheus rift basin. The basin geometry influenced deformation style by controlling the initial thickness of the massive lower Argo salt. Generally, the lower Argo salt is thin or absent above shallow fault blocks and thick above deep fault blocks. The composition of the upper Argo Formation, which consists of halite and interbedded clastic sedimentary rocks, also influenced the deformation style in the basin. In parts of the basin, the halite of the upper Argo Formation is interbedded with numerous, thick shale beds. In other parts of the basin, however, the upper Argo Formation is predominantly halite with few shale beds, allowing it to behave ductilely like the massive lower Argo salt. The synrift Argo salt significantly influenced deformation during and after rifting. Growth beds in the upper Argo Formation associated with extensional fault-propagation folds reflect continued activity on basement-involved faults below the salt during its deposition. During the later phases of rifting, paired minibasins and salt walls/columns preferentially formed where the lower Argo salt was thick and/or where the upper Argo Formation had a high proportion of halite. Sediment loading near the northern border faults caused the underlying salt to move laterally, forming the minibasins, salt walls/columns, and possibly detached compressional structures. Immediately after rifting, shortening associated with basin inversion reactivated some basement-involved faults. Detached compressional structures (i.e., salt-cored folds) located to the south and far from minibasins likely resulted from this basement-involved shortening. It is unclear whether the detached compressional structures near the minibasins formed, at least in part, in response to the basement-involved shortening. The nature of the widespread unconformity during the Late Jurassic/Early Cretaceous remains unclear. However, additional postrift deformation during the Oligocene/Miocene again reactivated some basement-involved faults and shortened the buried salt walls/columns, producing domes in the sedimentary cover above them.

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 categoriesScience and technology studies
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.067
Threshold uncertainty score1.000

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 studies0.0020.001
Scholarly communication0.0000.001
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 head0.003
GPT teacher head0.143
Teacher spread0.139 · 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