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Record W3145957772 · doi:10.7282/t3wd404m

The Mesozoic Orpheus rift basin, offshore Nova Scotia and Newfoundland, Canada

2011· article· en· W3145957772 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) · 2011
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological formations and processes
Canadian institutionsnot available
Fundersnot available
KeywordsRiftNova scotiaGeologyPaleontologyMesozoicStructural basinSubmarine pipelineOceanography

Abstract

fetched live from OpenAlex

The Orpheus rift basin of offshore eastern Canada formed during the Mesozoic breakup of the Pangean supercontinent before the opening of the North Atlantic Ocean. Using a dense grid of 2D seismic data, I have identified four distinct unconformity-bounded packages (A-D) associated with the basin’s early development. Information from nearby wells (albeit limited) and regional stratigraphy suggest that packages A, B, C, and D represent Paleozoic prerift strata and basement, Late Triassic (possibly Middle Triassic or Permian) to early Early Jurassic synrift strata, late Early to Middle Jurassic lower postrift strata, and Middle to Late Jurassic upper postrift strata, respectively. The synrift section contains salt and numerous igneous intrusions of the latest Triassic/earliest Jurassic Central Atlantic Magmatic Province (CAMP). Based on tectonostratigraphic analysis of the seismic data, I propose that the Orpheus and overlying Scotian basins experienced at least four stages of development during the Mesozoic. 1) Continental extension associated with rifting began by Late Triassic time (and possibly during Middle Triassic or Permian time) and continued into early Early Jurassic time, producing a series of E-striking, S-dipping basement-involved faults with normal separation (the Cobequid-Chedabucto border-fault system) that bound the Orpheus basin on the north. During early rifting, the basin was broad with few intrabasin faults. Most intrabasin, basement-involved faulting began during salt deposition, increasing the accommodation space and causing pronounced southward thickening of the salt. Movement on basement-involved faults during rifting produced broad fault-propagation folds in the synrift strata above the salt. 2) Shortening/inversion occurred shortly after rifting, causing widespread uplift and erosion and producing the breakup unconformity. Below the salt, the shortening reactivated many of the basement-involved extensional faults with at least a reverse component of displacement. Above the salt, the shortening produced salt-cored detachment folds and detached thrust faults. 3) Postrift thermal subsidence started likely by the late Early Jurassic, producing the Scotian postrift basin. Postrift salt movement resumed and continued until Late Jurassic, producing fault-parallel salt-cored highs and salt-withdrawal lows. 4) Regional uplift and erosion occurred during the latest Jurassic to Early Cretaceous, producing the widespread Avalon unconformity.

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: none
Teacher disagreement score0.863
Threshold uncertainty score0.998

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
Science and technology studies0.0030.001
Scholarly communication0.0000.001
Open science0.0010.000
Research integrity0.0000.001
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 head0.016
GPT teacher head0.155
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