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Record W7052012937

The orthogneiss-derived migmatites of the Variscan Ulten Zone, Northeastern Italy: limited magma movement through the lower crust

2011· article· en· W7052012937 on OpenAlexaboutno aff

Bibliographic record

VenueArchivio istituzionale della ricerca (Alma Mater Studiorum Università di Bologna) · 2011
Typearticle
Languageen
FieldEngineering
TopicPlasma Diagnostics and Applications
Canadian institutionsnot available
Fundersnot available
KeywordsMigmatitePartial meltingResiduumMagmaGneissCrustMelt inclusionsMetamorphic rockPlagioclase
DOInot available

Abstract

fetched live from OpenAlex

Anatectic melt (or magma) created in migmatites, is potentially mobile (Sawyer 2008). The Variscan Ulten Zone, on the contrary, provides an example of limited melt transfer within a km-sized lower crust. In the southern side of the Maddalene, the mountain range that straddles the Ulten and Non Valleys of Northeastern Italy, the high-grade basement of the Ulten Zone is dominated by metapelite-derived stromatic to nebulitic migmatites with intercalated minor granitic orthogneisses. In this area we have successfully recognized different stages of partial melting within the orthogneisses. The source rock of the orthogneiss-derived migmatites is a leucocratic gneiss made of alkali-feldspar + quartz + plagioclase and white mica (up to 12 vol%), and accessory biotite, garnet and ilmenite. The migmatites are characterised by the occurrence of patch or layers of felsic and isotropic leucosome. In the migmatites, the residuum contains skeletal grains of white mica, suggesting that the breakdown of white mica controlled the partial melting process. Thermodynamic modelling indicates that the complete consumption of white mica produces a melt fraction of 5%. The major-element chemical composition of the orthogneiss-derived migmatites is similar to that of the orthogneiss source rock, thus supporting the hypothesis that the partial melting of the Ulten orthogneiss occurred without, or limited, removal of material. Correspondingly, the stromatic to nebulitic migmatites produced by 20-30% partial melting of the Ulten metapelites (Braga, Massonne in press) have a composition consistent with their source rocks.\nThe observations from the Variscan Ulten Zone suggest that the melt fraction in a deep crust is not always capable of migrating away from the source region. The occurrence of a melt-rich lower crust during orogenic evolution decreases the strength of the thickened crust thus favouring the gravitational collapse of mountain belts (Vanderhaeghe, Teyssier 2001).\n\nReferences:\nBRAGA R., MASSONNE H.-J., in press: H2O content of deep-seated orogenic continental crust: the Ulten Zone, Italian Alps. Int. Geol. Rev.\nSAWYER E.W., 2008: Working with migmatites: nomenclature for the constituent parts, Mineralogical Association of Canada Short Course, 38: 1-28.\nVANDERHAEGHE O., TEYSSIER C., 2001: Partial melting and flow of orogens. Tectonophysics, 342: 451-472.

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 score0.786
Threshold uncertainty score0.808

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 studies0.0010.000
Scholarly communication0.0000.000
Open science0.0010.001
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 head0.014
GPT teacher head0.194
Teacher spread0.180 · 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".

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Citations0
Published2011
Admission routes1
Has abstractyes

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