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Record W1588744200 · doi:10.1029/gm050p0101

Refinements of the “Baja British Columbia” Plate-Tectonic Model for Northward Translation Along the Margin of Western North America

2011· book-chapter· en· W1588744200 on OpenAlexaboutno aff
Paul J. Umhoefer, Joe D. Dragovich, Jeff Cary, David C. Engebretson

Bibliographic record

VenueGeophysical monograph · 2011
Typebook-chapter
Languageen
FieldEarth and Planetary Sciences
TopicGeology and Paleoclimatology Research
Canadian institutionsnot available
FundersNational Science Foundation
KeywordsPaleomagnetismGeologyTerranePlate tectonicsNorth American PlatePacific PlateCretaceousSeismologyPaleontologyTectonicsGeodesySubduction

Abstract

fetched live from OpenAlex

Paleomagnetic data suggest that a large part of northern Washington, British Columbia, the Yukon, and southern Alaska (as a whole block named Baja British Columbia or Baja BC) was at the paleolatitude of Mexico at about 90 Ma. Additional paleomagnetic data show that Baja BC was in place relative to cratonic North America by about 55 Ma. We assume that Baja BC was adjacent to North America by middle Cretaceous time, and was driven northward by Kula (and/or Farallon)-North America plate interactions from 90 to 56 Ma. Terrane-travel analysis based on the fixed hot-spot hypothesis shows that the Kula plate could have driven Baja BC the distance inferred from the paleomagnetic data from the Spuzzum and Mount Stuart plutons in the interval from 90 to 68 Ma. A model with a north-south boundary between the Kula and North America plates produces sufficient latitudinal displacement even when the component of movement parallel to the coast is as low as 50%. A north-south plate boundary between the Farallon and North America plates also produces sufficient latitudinal displacement to move Baja BC the inferred distance. The Farallon-North America model, however, only is viable in the extreme case when all of the plate motion was coast-parallel and the entire 90 to 56 Ma time interval is used. In our preferred scenario for translation of Baja BC, the southern end of the block was at the paleolatitude of west central Mexico at 85 Ma, after a few hundred kilometers of translation along the Farallon-North America plate margin. Baja BC then moved along a north-south transform fault(s) between the Kula and North America plates from 85 to 74 Ma, and along an oblique-convergent margin from 74 to 66 Ma. By about 70 Ma the southern part of Baja BC was at the paleolatitude of Oregon, just north of the Klamath Mountains. A triple-junction analysis shows that the Kula-Farallon-North America triple junction would also move rapidly northward in the wake of Baja BC. Most of the possible variations in the type of triple junction place it along northern California by 70 Ma, suggesting that the Kula plate would be offshore of the region from California to southwestern Mexico for part of the 85- to 70-Ma interval, and that the Farallon plate would be adjacent to southwestern North America both preceding and following the interaction of the Kula plate.

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)0.001
metaresearch head score (Gemma)0.002
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Not applicable · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.313
Threshold uncertainty score0.630

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0010.002
Meta-epidemiology (narrow)0.0010.001
Meta-epidemiology (broad)0.0000.001
Bibliometrics0.0010.001
Science and technology studies0.0020.001
Scholarly communication0.0020.001
Open science0.0020.001
Research integrity0.0010.001
Insufficient payload (model declined to judge)0.0050.001

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 head0.032
GPT teacher head0.213
Teacher spread0.181 · 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 designNot applicable
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

Citations13
Published2011
Admission routes1
Has abstractyes

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