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Record W7115817144

Facies architecture, paleodischarge, and the variability of confluence scours in Cretaceous Rivers: Ferron Sandstone, Utah and Torrivio Sandstone, New Mexico, USA

2025· dissertation· en· W7115817144 on OpenAlexfundno aff

Bibliographic record

VenueMacSphere (McMaster University) · 2025
Typedissertation
Languageen
FieldEarth and Planetary Sciences
TopicGeological formations and processes
Canadian institutionsnot available
FundersNatural Sciences and Engineering Research Council of CanadaMcMaster University
KeywordsFluvialConfluenceFaciesTributaryCretaceousAquifer
DOInot available

Abstract

fetched live from OpenAlex

This thesis is focused on the integration of facies architectural analysis with 3D drone imagery, to provide quantitative analysis of ancient North American Cretaceous river systems. Paleo-digital elevation models were used for estimating drainage area, consistent with previous paleogeographic reconstructions. Monte-Carlo simulations, in combination with physics-based, empirically-derived equations, were used to estimate paleodischarge and downstream sediment volumes. This represents novel use of datasets and methods in quantitative estimation of ancient fluvial systems. This quantitative approach has broad implications for source-to-sink scaling relationships, such as predicting ancient drainage areas, that can be important in paleotectonic and paleogeographic reconstructions, as well as prediction of downstream sink volumes, which have economic importance, as these estimations can be used in hydrocarbon exploration in predicting the volumes of both the reservoir as well as the source rocks. These are also useful for characterizing aquifers to assess aquifer volume and flow pathways. This thesis also addresses a number of on-going scientific debates. The lack of braided rivers imaged using 3D seismic data has raised questions about the preservability of braided river deposits. This thesis provides an unequivocal example of a braided fluvial system from the late Cretaceous Torrivio Sandstone in New Mexico, USA. There is also some debate on how to distinguish autogenic scours from allogenic scour surfaces in ancient systems, with implications for identifying regional sequences. This thesis presents examples of a wide variety of autogenic fluvial scour surfaces, including bar-top hollows, bar-scale confluence scours and channel scours, ranging from normal small-scale channel confluence scours to larger tributary junction scours. The criteria described in this thesis enable the distinction of autogenic scours from regional allogenic incised valley surfaces that define sequence boundaries. The thesis also addresses the long debated concept of “Big River” systems. Integration of qualitative facies architecture analysis with quantitative estimates, derived using novel datasets and methods, show that the scale of major depositional elements can be used to estimate the size and scale of formative rivers and help to distinguish deposits of continental-scale river systems from the smaller rivers documented herein.

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)0.001
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 score0.230
Threshold uncertainty score0.457

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.001
Science and technology studies0.0000.000
Scholarly communication0.0010.000
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 head0.011
GPT teacher head0.201
Teacher spread0.190 · 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
Published2025
Admission routes1
Has abstractyes

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