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Preservation of igneous and metamorphic charnockites in the Paleoproterozoic Prøven Igneous Complex, Rinkian Orogen, central West Greenland

2024· article· en· W4404873618 on OpenAlexaboutno aff
Annika Dziggel, L. Bramm, Thomas F. Kokfelt, John Grocott, Johann F.A. Diener

Bibliographic record

VenuePrecambrian Research · 2024
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsnot available
Fundersnot available
KeywordsIgneous rockGeologyMetamorphic rockGeochemistryVenCharnockiteGneissAnatexisPartial meltingGeomorphologyGranuliteCrustHumanitiesFacies

Abstract

fetched live from OpenAlex

• Prøven igneous complex preserves igneous and metamorphic charnockites. • Emplacement occurred at relatively shallow crustal levels. • Magmatism was accompanied by high-grade metamorphism. • Related to the collision of the Meta Incognita microcontinent and the Rae Craton. The Paleoproterozoic Prøven Igneous Complex (PIC) of the Rinkian Orogen in central West Greenland comprises a suite of arc-related charnockite plutons, extending over an area of at least 7200 km 2 . The PIC was emplaced into paragneisses of the Karrat Group during a series of magmatic events between c. 1900 and 1850 Ma. Magmatism was accompanied by high-grade metamorphism and deformation, culminating in granulite facies peak conditions and partial melting at c. 1820 Ma. To unravel the conditions of charnockite formation and granulite facies metamorphism, a detailed petrographic study was carried out on samples from the PIC and the surrounding paragneisses. The rock types studied include i) charnockites from the massive PIC, ii) charnockites and migmatites from the layered lower PIC, iii) migmatites from the surrounding paragneisses, and iv) igneous enclaves from the lower PIC. Charnockites from the massive PIC generally show a magmatic, porphyritic texture and only minor macro-textural evidence of deformation. The lower PIC and paragneisses are both migmatized and exhibit extensive recrystallization with a solid-state crystal-plastic fabric. Igneous enclaves are found within the lower PIC and show an equigranular, igneous texture. Based on the dominant igneous texture it is interpreted that the massive PIC crystallized from a dry magma and was not significantly overprinted during peak metamorphism. Phase equilibrium modelling, Hb-Pl thermometry and Al-in-hornblende barometry constrain the PIC to have been emplaced at 680–795 °C and 4.2–5.4 kbar. By contrast, the lower PIC and paragneiss samples record granulite facies peak conditions of 785–805 °C and 3.4–4.0 kbar, suggesting that both charnockite magmatism and metamorphism took place at relatively shallow crustal levels. Our results are consistent with the P-T conditions recorded by the 1890–1880 Ma Qikiqtarjuaq Plutonic Suite, an arc-type charnockite intrusion on Baffin Island, Canada. A correlation between the tectonothermal events on Baffin Island and in the Rinkian Orogen is proposed, therefore relating the intrusion of the PIC to the collision of the Meta Incognita microcontinent and the Rae Craton.

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)0.001
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesInsufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.043
Threshold uncertainty score0.998

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.000
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 science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0030.000

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 head0.088
GPT teacher head0.297
Teacher spread0.209 · 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.

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".

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Citations1
Published2024
Admission routes1
Has abstractyes

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