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Record W7008633018

Continental Breakup, Mountain Building, and the Great Unconformity: The Exhumation History of North America’s Most Iconic Erosional Surface Using Zircon (U-Th)/He Thermochronology

2024· dissertation· en· W7008633018 on OpenAlexaboutno aff

Bibliographic record

VenueCU Scholar (University of Colorado Boulder) · 2024
Typedissertation
Languageen
FieldEarth and Planetary Sciences
TopicPaleontology and Stratigraphy of Fossils
Canadian institutionsnot available
Fundersnot available
KeywordsThermochronologySupercontinentRodiniaProterozoicUnconformitySedimentary rockZirconSnowball EarthPaleozoic
DOInot available

Abstract

fetched live from OpenAlex

The Proterozoic and early Paleozoic is a key period in Earth’s history coincident with the amalgamation and breakup of the supercontinent Rodinia, global Snowball Earth glaciations, oxygenation of the atmosphere and deep oceans, and the Cambrian Explosion of biological diversity. However, the global sedimentary record is sparse prior to the Cambrian, making investigations of this time period difficult. Around the globe, Phanerozoic sedimentary rocks unconformably overlie Proterozoic and older igneous and metamorphic “basement” rocks, representing 300 million to over one billion years of Earth history depending on location. On North America, this unconformable contact is called “the Great Unconformity” and is observed across the continent. Despite the limited Proterozoic sedimentary rock record, we can still learn a great deal about processes on Earth’s surface during this time from the rocks that are preserved. This dissertation presents three applications of (U-Th)/He thermochronology to understanding the timing and mechanisms by which rocks were exhumed and eroded to expose Proterozoic basement, create the Great Unconformity, and provide sediment for sedimentary basins. Applications of (U-Th)/He thermochronology to exhumation focus on constraining the timing, magnitude, and associated mechanisms of Great Unconformity exhumation in the Grand Canyon, USA and southeastern Ontario, Canada. New (U-Th)/He thermochronologic data combined with independent field evidence and geochronologic data reveal distinctly different timings of exhumation in these locations. In the Grand Canyon, Great Unconformity exhumation reflects paleotopographic evolution related to Rodinia assembly and breakup. In Ontario, significant exhumation occurs in the Ediacaran to Cambrian, associated with temporally long-lived geodynamic and tectonic processes impacting the Canadian Shield. (U-Th)/He thermochronology is also applied to understanding exhumation of sediment and deposition in the Neoproterozoic Jacobsville Sandstone, located on the Upper Michigan Peninsula, USA and associated with the c. 1090-980 Ma Grenville Orogeny and amalgamation of Rodinia. The dataset presented here suggests at least five periods of exhumation contributing sediment, hinting at surface processes that may have been active on the continental interior of Rodinia.

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 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 categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.594
Threshold uncertainty score0.996

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0010.002
Scholarly communication0.0000.000
Open science0.0010.000
Research integrity0.0000.001
Insufficient payload (model declined to judge)0.0000.000

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 head0.012
GPT teacher head0.209
Teacher spread0.196 · 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 teacher head, 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
Published2024
Admission routes1
Has abstractyes

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