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Record W3108233830 · doi:10.1306/12401042st563288

Chapter 128: Stratigraphic Architecture and Depositional Processes of a Proximal Crevasse Splay and Genetically Related, Sinuous Channel Fill, Isaac Formation, British Columbia, Canada

2007· article· en· W3108233830 on OpenAlexaboutno aff
R. W. C. Arnott

Bibliographic record

Venuenot available
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological formations and processes
Canadian institutionsnot available
Fundersnot available
KeywordsGeologyCrevasseOverbankTurbiditeGeomorphologySedimentary depositional environmentGeochemistrySedimentary structuresLeveePaleontologySedimentary rockGeotechnical engineeringStructural basin

Abstract

fetched live from OpenAlex

Abstract Channel-fill and adjacent lithofacies are well exposed in the deep-marine Neoproterozoic Windermere Supergroup. At one location, levee deposits are overlain by a proximal crevasse splay, which is overlain by a channel-fill complex. Levee deposits, which consist of thin-bedded, Tcd- or Tcde-division turbidites interstratified with thicker, coarser grained, more complete (Tabcd-division) turbidites (overbank splay deposits), accumulated adjacent to an active channel. Levee strata are overlain abruptly by a 23-m (75-ft)-thick, proximal-crevasse-splay deposit. The splay was initiated by avulsion of an adjacent, previously active channel. Energetic turbulent suspensions, now diverted through the levee and into the interchannel area, expanded rapidly, lost capacity, and incrementally constructed the crevasse splay. Depending on the rate of turbulent-suspension collapse, two lithofacies were deposited: (1) medium-bedded, fine- to medium-grained sandstone Tcd turbidites deposited by low-concentration dispersions, or (2) medium-bedded, coarse-tailed-graded, structureless, medium-grained sandstone deposited rapidly in submerged hydraulic jumps (turbidites were deposited from reconstituted dispersions that formed along the periphery of the jump). The intercalation of turbidites and structureless sandstones probably indicates lateral migration of the hydraulic jump and consequent compensational stacking of the two lithofacies. Splay deposits are overlain erosively by a ~14 m (~46 ft) channel-fill complex comprising two channel fills; the channel fills are separated by a zone with abundant mudstone intraclasts. Intraclasts may represent the eroded remnants of a mud plug deposited during the final stages of channel 1 (C1) fill that subsequently became eroded during the inception of channel 2 (C2). Both channel fills consist of medium- to thick-bedded, normally graded, coarse- to very coarse-grained sandstone and granule conglomerate that show a poorly developed fining-upward but better developed thinning-upward trend. Both channel fills show well-developed lateral accretion surfaces, suggesting that the channels had a sinuous planform.

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 score0.015
Threshold uncertainty score0.101

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0030.004
Science and technology studies0.0020.001
Scholarly communication0.0010.000
Open science0.0010.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0040.000

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 head0.005
GPT teacher head0.162
Teacher spread0.157 · 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
Published2007
Admission routes1
Has abstractyes

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