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Record W1589680485 · doi:10.2110/pec.06.85.0219

Delta-Plain Paleodrainage Patterns Reflect Small-Scale Fault Movement and Subtle Forebulge Uplift

2006· book-chapter· en· W1589680485 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

VenueSEPM (Society for Sedimentary Geology) eBooks · 2006
Typebook-chapter
Languageen
FieldEarth and Planetary Sciences
TopicGeological formations and processes
Canadian institutionsnot available
Fundersnot available
KeywordsForeland basinGeologyCretaceousPaleontologyDeltaStructural basinFault (geology)Scale (ratio)GeographyCartographyEngineering

Abstract

fetched live from OpenAlex

Abstract: The extreme sensitivity of rivers to subtle changes of slope resulting from tectonic tilting provides a basis for the interpretation of four Cretaceous paleovalley systems mapped on four successive sequence-bounding surfaces in the mid-Cenomanian Dunvegan Formation, deposited in the foredeep of the Western Canada Foreland Basin. The northern part of the study area overlies the Peace River Arch, a long-lived structural entity that is transected by faults trending dominantly NW–SE and NE–SW. The Dunvegan Fm. comprises a series of at least ten deltaic sequences labeled J–A in ascending order, and each spans ~ 100–200 ky. Valleys mapped on the top of sequences F, G, and H have many straight reaches that tend to parallel the rectilinear fault pattern in the underlying Paleozoic rocks, and many reaches are colinear with deep-seated faults. There is no evidence for deflection of rivers along the axis of the foreland basin. Isopach maps show that sequences H, G, and F do not thicken appreciably into the foredeep, suggesting that the contemporaneous rate of plate flexure was low. In-plane stress level is also inferred to have been low. Under these conditions, the forebulge was suppressed and long-lived faults in the Peace River Arch area were “unlocked”, permitting individual blocks to undergo vertical isostatic adjustment on a scale of meters. The low-gradient coastal-plain rivers were strongly influenced by this tectonic topography. In contrast, sequences E–A show marked westward thickening into a newly developed foredeep. Paleovalleys on sequence E do not have a preferred rectilinear pattern, instead being dominantly dendritic; distally, valleys are abruptly deflected to flow parallel to the basin axis. This new paleodrainage pattern is interpreted to reflect subtle uplift of a forebulge in response to renewed plate flexure, causing river deflection to the SE. The level of in-plane stress is inferred to have increased at this time, “locking” faults over the Arch and causing the land surface to deform as a regionally homogeneous plane, favoring dendritic drainage. The inferred position of the forebulge approximates the position of a long-lived Cretaceous paleodrainage divide and also coincides with a terrane suture in the Precambrian basement. The suture is inferred to have been a lithospheric weak zone, repeatedly serving to localize the forebulge. Although vertical displacement on both faults and forebulge cannot conclusively be recognized in cross sections or isopach patterns, it appears that rivers were readily diverted by these extremely subtle topographic features.

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 categoriesMeta-epidemiology (narrow), Insufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Not applicable · Consensus signal: none
GenreCandidate signal: Other · Consensus signal: Other
Teacher disagreement score0.574
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0010.001
Meta-epidemiology (broad)0.0010.001
Bibliometrics0.0000.000
Science and technology studies0.0010.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0010.001
Insufficient payload (model declined to judge)0.0020.000

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 head0.210
Teacher spread0.194 · 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