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Record W2802687689 · doi:10.7939/r3kd89

Stratigraphy, paleogeography and tectonic evolution of early Paleozoic to Triassic pericratonic strata in the northern Kootenay Arc, southeastern Canadian Cordillera, British Columbia

2013· article· en· W2802687689 on OpenAlex
Jamie L Kraft

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

VenueUniversity of Alberta Library · 2013
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsnot available
Fundersnot available
KeywordsPalaeogeographyGeologyPaleozoicStratigraphyPaleontologyTectonicsArc (geometry)Island arcVolcanismSubduction

Abstract

fetched live from OpenAlex

The northern Kootenay Arc in southeastern British Columbia hosts a near-continuous succession of Cambrian to Permian strata that were deposited in overlapping marginal basins outboard of the Canadian Cordilleran miogeocline. The basinal strata of the Late Cambrian and younger Lardeau Group are conformably overlain by a succession of Devonian and Early Mississippian strata herein named the Mount Sproat assemblage. The Mount Sproat assemblage comprises an undated carbonaceous lower unit that passes upward into a lithologically diverse succession of siliciclastic, carbonate and mafic metavolcanic strata that have geochemical signatures recording a transition from non-arc to arc-related volcanism. Calc-alkaline basalt in the Mount Sproat assemblage yielded prismatic zircon dated at 367.2 ± 2 Ma. The Mount Sproat assemblage is truncated by an angular unconformity at the base of the Late Mississippian Milford Group. Lower stratigraphic levels of the Mount Sproat assemblage were deformed penetratively with the Lardeau Group prior to deposition of the Milford Group. The Thompson assemblage (new term) is a localized sedimentary succession between the Viséan Milford Group and the Broadview Formation (Lardeau Group) at Mount Thompson. It was deposited after Early Mississippian deformation of the Lardeau Group and was partially eroded into the overlying the Milford Group. Detrital zircon dates in the intervals 2.8-2.6 Ga and 2.1-1.75 Ga link the Lardeau Group, Mount Sproat assemblage, Thompson assemblage and Milford Group to the Canadian Cordilleran miogeocline. Detrital zircon data also reveal sources of zircon that were not available to the miogeocline. The Broadview Formation is interpreted to record uplift of an outer high of sialic North American crust that contained zircon in the intervals 1.48-1.41 Ga, 1.38-1.32 Ga, and 1.30-0.95 Ga in addition to ages typical of the adjacent miogeocline. Palinspastic restoration of this margin places the edge of attenuated North American cratonic crust near the present day coastline of southern British Columbia. In Late Devonian to Late Triassic time, detrital zircon grains with Neoproterozoic (700-550 Ma) and Silurian (ca. 420 Ma) dates appear in the dataset. These dates are interpreted to originate from an exotic terrane that docked in mid-Devonian time.

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 categoriesInsufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.026
Threshold uncertainty score0.989

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 studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0120.000

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 head0.129
Teacher spread0.125 · 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