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Record W7145284848

U-Pb zircon ages of Early Archean gneisses from northern Labrador

2012· article· en· W7145284848 on OpenAlexaboutno aff
伸次 山本, shinji yamamoto, 岳史 平田, TAKAFUMI HIRATA, 佑介 澤木, 一勝 青木, K. Aoki, 吉弘 岡田, Yoshihiro Okada, 剛 小宮, Tsuyoshi Komiya

Bibliographic record

VenueInstitutional Repositories DataBase (IRDB) · 2012
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsnot available
Fundersnot available
KeywordsZirconGneissArcheanProtolithCratonMetamorphic rockMigmatiteAnatexis
DOInot available

Abstract

fetched live from OpenAlex

Early Archean crustal records are rare, but contiguous units are best preserved in N. Labrador and the NWT (Canada) and in SW Greenland. The Saglek-Hebron area (N. Labrador), located at the W. extension of the North Atlantic Craton (NAC), contains wellpreserved Eo-Paleoarchean suites including pre-3.8 Ga Nanok Ferich monzodioritic gneiss, the Nulliak supracrustal assemblage (ca. 3.8 Ga), 3.7-3.6 Ga Uivak I TTG gneisses, 3.5-3.4 Ga Uivak II augen gneisses and Mesoarchean 3.2 Ga Lister gneiss [1-3]. Saglek dykes are present in the Eo and Paleoarchean gneisses, but not in the younger Lister gneisses. Despite confirmation of the antiquity of the area [3,4] a comprehensive zircon U-Pb dating with LA-ICPMS employing cathodluminescence (CL) imaging has not been undertaken for orthogneisses and supracrustal suites. CL images are essential to discuss inherited grains, pristine core and overgrowth. We conducted LA-ICPMS U-Pb geochronological study of zircons from TTG Uivak I gneiss from the Saglek-Hebron area. The CL images of zircon grains display internal structures of oscillatory zoning and homogeneous core with overgrowth rim. Results show that samples collected as Uivak I TTG gneisses can be classified into three groups based on the distribution of zircon ages. The first group of TTGs is characterized by both presence of older zircons than 3.8 Ga, with the maximum age of 3914 ± 40 Ma in 207Pb/206Pb age, and apparent lack of 3.6 to 3.8 Ga zircons. These are obviously members of the Nanok gneiss. Based on intrusive relationships observed in the field, the Nanok gneiss is pre-date emplacement of the protoliths of the Uivak I gneisses. The second and third groups have clear peaks at 3.7-3.6 Ga and ca. 3.3 Ga in their age distribution of zircon cores, indicating that TTGs of the second and third groups correspond to Uivak I gneiss and the Lister gneiss, respectively. Importantly, overgrowth rims of zircons we analyzed here show ca. 2.7 Ga, which reflect zircon growth during late Archean thermal event in the NAC, possibly associated with assembly of different terranes within the gneiss complex. We show that the combination of in-situ U-Pb dating and CL imaging can reveal the tectonothermal history of early Archean from the gneisses in N. Labrador.

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: Bench or experimental · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.574
Threshold uncertainty score0.846

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0030.003
Science and technology studies0.0010.000
Scholarly communication0.0010.000
Open science0.0010.001
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.001

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 head0.019
GPT teacher head0.217
Teacher spread0.198 · 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 designBench or experimental
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
Published2012
Admission routes1
Has abstractyes

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