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Record W7046568881

Detrital Zircon U-Pb Geochronology of Upper Mississippian Siltstone, Oklahoma and Arkansas

2021· article· en· W7046568881 on OpenAlexaboutno aff

Bibliographic record

VenueJournal of the Arkansas Academy of Science · 2021
Typearticle
Languageen
FieldPhysics and Astronomy
TopicMagnetic confinement fusion research
Canadian institutionsnot available
Fundersnot available
KeywordsZirconGeochronologyProvenanceSiltstoneDetritusPaleocurrentLaurentiaSedimentary rock
DOInot available

Abstract

fetched live from OpenAlex

Although Upper Mississippian strata have been characterized extensively using lithostratigraphy, sequence stratigraphy, and biostratigraphy across the North American midcontinent, the origin of the silt comprising the Meramec STACK (Sooner Trend Anadarko Basin, Canadian and Kingfisher counties) reservoirs of the Anadarko Basin in west-central Oklahoma and age equivalent units is not well understood, despite its economic importance as an unconventional petroleum reservoir. Previously published models have variously invoked fluvial, marine, and aeolian sediment transport for Upper Mississippian siltstone present along the paleo-shelf edge of the Laurentian craton. This study uses detrital zircon U-Pb geochronology and grain morphology, handheld x-ray fluorescence (hXRF) whole rock geochemistry, and petrography to constrain sediment provenance of Upper Mississippian (Meramecian and Chesterian) strata along the Laurentian paleo-shelf edge. Conservative mineral separation techniques were developed to facilitate processing of silt-sized material, allowing efficient recovery in small (i.e., <100 >g) samples. Detrital zircon U-Pb age and grain morphology data reported in this study indicate that Upper Mississippian silt-sized detritus was not only sourced from to Laurentia but was also sourced from advancing peri-Gondwanan terranes to the south and/or east. Of the 2478 detrital zircon analyses measured from nineteen Meramecian siltstone samples, 32% were Grenville (900-1350 Ma), 21% were Appalachian (240-500 Ma), and 17% were peri-Gondwanan (500-900 Ma). Zircon grain size and morphology data complements U-Pb age data and provides additional insight into potential sediment transport mechanisms of the Meramecian silt. Peri-Gondwanan detrital zircons (500-900 Ma) are smaller and more spherical than Appalachian (240-500 Ma) or Grenville (900-1300 Ma) zircon, suggesting that these peri-Gondwanan grains may have traveled greater distances. Age-equivalent samples on the craton of Laurentia do not possess a significant component of 500-900 Ma zircon, suggesting peri-Gondwana grains along the paleo-shelf edge were transported via marine currents rather than by wind. The combination of detrital zircon U-Pb ages, morphology data, and petrographic observations support a model for long-distance transport of peri-Gondwanan zircon to the southern Laurentian margin via contour-parallel marine currents. These far travelled grains mixed with detritus sourced from the easterly Appalachian Orogeny along the southern paleo-shelf edge of Laurentia. This study documents a significant peri-Gondwanan influence in the southern midcontinent of North America during Meramecian time, the presence of which predates the consequent arrival of these southerly terranes during the collision of southern Laurentia with Gondwana.

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 score0.173
Threshold uncertainty score0.343

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.001
Science and technology studies0.0010.000
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 head0.012
GPT teacher head0.280
Teacher spread0.268 · 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
Published2021
Admission routes1
Has abstractyes

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