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Record W1512965500

The Black Hills: a keystone of North American continental evolution for over 2.6 billion years

2006· article· en· W1512965500 on OpenAlexaboutno aff
Mary S. Hubbard, P. S. Dahl, Guy S. Duke, E. F. Duke, Peter I. Nábělek

Bibliographic record

VenueDigital Commons - USU (Utah State University) · 2006
Typearticle
Languageen
FieldComputer Science
TopicGeochemistry and Geologic Mapping
Canadian institutionsnot available
Fundersnot available
KeywordsKeystone speciesGeographyEcologyBiology
DOInot available

Abstract

fetched live from OpenAlex

The Black Hills region provides an excellent field laboratory to study numerous aspects of the continental evolution of North America from the Neoarchean to the Recent. The Neoarchean basement consists of 2.60- 2.56 Ga gneissic granitoids that formed during an early episode of convergent thermotectonism. In the Paleoproterozoic the region experienced rifting at 2.48-1.98 Ga and renewed convergence at 1.75-1.71 Ga associated with early breakup and final reassembly of the Wyoming and Superior cratons, respectively. The product of this cratonic reconfiguration was a broad deformation zone known as the Trans-Hudson Orogen. Thermotectonic activity within the Dakota segment of this zone occurred at ~1820-1680 Ma compared to ~1860-1790 Ma in the Canadian segment. South of the Black Hills region the Yavapai (Central Plains) province was also accreted during the Precambrian. An extensive sequence of Cambrian through Cretaceous marine and continental sediments were laid down before the Black Hills were uplifted during the Laramide orogeny, which exposed the Precambrian crystalline core and its structures that record evidence for the major episodes of compressional deformation and intervening rifting events noted above. Laramide deformation may have actually localized along the Precambrian structures. Alkalic extrusive and intrusive activity occurred during late Laramide stages (~58 Ma) and continued up until ~46 Ma. Aeromagnetic evidence indicates that these mantle-derived magmas intruded along a N70°W trending fault with 50 km of left-lateral offset on the Precambrian surface. The Black Hills also sits astride the transition from the Rocky Mountain region to the northern Great Plains. South of the Black Hills there is evidence from fission track and stream deposition /erosion that the transition has been uplifting during the past 5 Ma. Other geophysical anomalies exist in the region including the North American Central Plains conductivity anomaly within the Trans Hudson Orogen and the South Dakota Gravity Low/High Heat Flow anomaly to the east of the Black Hills. These zones are possibly explained by ore deposition and fluid migration, respectively. Because of the extensive history of the Black Hills region, the exposure of an array of rock types/ages, and the presence of several anomalous geophysical zones, the Black Hills swath has been proposed as an area in which to establish a portion of the "geological framework" of North America through the integration of multiple geological and geophysical techniques during the EarthScope initiative.

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: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.315
Threshold uncertainty score0.403

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0010.000
Research integrity0.0000.000
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 head0.007
GPT teacher head0.181
Teacher spread0.174 · 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
Published2006
Admission routes1
Has abstractyes

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