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Record W4400842651 · doi:10.1130/b37239.1

Age, sedimentology, and deformational history of the Mesozoic Franciscan accretionary complex, Angel Island, California, USA

2024· article· en· W4400842651 on OpenAlexaff
Meghomita Das, Owen A. Anfinson, C. D. Rowe, Nicolas Schroeder

Bibliographic record

VenueGeological Society of America Bulletin · 2024
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological formations and processes
Canadian institutionsMcGill University
Fundersnot available
KeywordsSedimentologyMesozoicGeologyPaleontologyArchaeologySeismologyGeography

Abstract

fetched live from OpenAlex

Abstract The Franciscan Complex represents the forearc accretionary wedge that formed during late Mesozoic–Cenozoic subduction in California, USA, and preserves detailed records of long-lived subduction and exhumation of high-pressure, low-temperature rocks. As one of the world’s largest exposed subduction complexes, it records the evolution of subduction dynamics that correspond to the tectonic development of the western USA. Lithotectonic units within the Franciscan Complex represent different stages, mechanisms, and depths of accretion in the subduction history. Previous authors have proposed subdivisions for the Franciscan Complex, but as the metasedimentary units are very similar over large spatial and temporal scales, they have been difficult to map except on the broadest scales. This restricts the potential for researchers to characterize past tectonic events and subduction/exhumation mechanisms. Angel Island in the San Francisco Bay has previously been mapped as an undivided blueschist-facies metasedimentary unit thrust over lower-grade metasediments along the Quarry Point thrust, but we find that the Angel Island units include lithologic and metamorphic diversity spanning nearly the entire range of variability for the Franciscan Complex. We present new mapping, lithologic descriptions, and detrital zircon U-Pb geochronology to propose a new lithostratigraphy for Angel Island consisting of seven structurally juxtaposed units ranging from sub-metamorphic to low blueschist. The structurally highest and structurally lowest units are sub-blueschist grade, and the center of the fault-bounded stack consists of blueschist-grade metasediments separated by a thin sliver of sodic-amphibole metabasalt. The blueschist units and structurally higher sub-blueschist–grade units have maximum depositional ages of ca. 108–110 Ma, which is consistent with similar grade units from across the Bay Area, and they match well with respect to lithology and metamorphic grade. The structurally lowest units below the Quarry Point thrust have similar provenance but younger maximum depositional ages of ca. 97 Ma. These units have been suggested by previous authors to be affiliated with either Alcatraz or Marin Headlands rocks, which have similar depositional ages but show much more diversity in detrital zircon age spectra, which makes their association debatable. These results offer the first high-resolution detrital zircon U-Pb geochronologic dataset from the Franciscan Complex that allows definition of the diversity of age and provenance within a previously defined regional unit, which should be considered in future work attempting regional correlations with regional sample distribution.

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 score0.623
Threshold uncertainty score0.759

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.002
Science and technology studies0.0010.000
Scholarly communication0.0010.000
Open science0.0010.000
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 head0.018
GPT teacher head0.208
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

Citations2
Published2024
Admission routes1
Has abstractyes

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