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Record W1974553500 · doi:10.1086/600862

Petrogenetic and Metallogenetic Relationships in the Eastern Cordillera Occidental of Central Peru

2009· article· en· W1974553500 on OpenAlexaff
Thomas Bissig, Richard M. Tosdal

Bibliographic record

VenueThe Journal of Geology · 2009
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsUniversity of British Columbia
Fundersnot available
KeywordsGeologyIgneous rockGeochemistryRadiogenic nuclidePetrogenesisGeochronologyIsotopes of strontiumSedimentary rockMagmatismStrontiumTectonicsMantle (geology)PaleontologyPhysics

Abstract

fetched live from OpenAlex

Ore deposits spatially and temporally related to high‐K calc‐alkaline intrusions or domes are widespread in the central Peruvian Cordillera Occidental. Geochronology and petrochemistry of intrusive rocks associated with mineralization reveal that most ore deposits (1) were emplaced in the late Middle to early late Miocene and (2) are related to calc‐alkaline igneous rocks of granodioritic composition with $$\mathrm{Sm}\,/ \mathrm{Yb}\,> 3$$ , $$\mathrm{Sr}\,/ \mathrm{Y}\,> 40$$ , and $$\mathrm{Y}\,/ \mathrm{Th}\,< 1.5$$ . The largest deposits are associated with intrusions with $$\mathrm{Sm}\,/ \mathrm{Yb}\,> 4$$ . Strontium isotopic compositions of the igneous rocks vary from $$^{87}\mathrm{Sr}\,/{}^{86}\mathrm{Sr}\,=0\mathrm{.}\,7038$$ to 0.7089, but the $$^{87}\mathrm{Sr}\,/ {}^{86}\mathrm{Sr}\,$$ ratio values exhibit only a poorly defined overall trend toward increased crustal contamination through time. Lead isotopic ratios generally correlate with the Sr isotopes and range from $$^{206}\mathrm{Pb}\,/ {}^{204}\mathrm{Pb}\,=18.64$$ to 18.91, from $$^{207}\mathrm{Pb}\,/ {}^{204}\mathrm{Pb}\,=15.58$$ to 15.66, and from $$^{208}\mathrm{Pb}\,/ {}^{204}\mathrm{Pb}\,=38.60$$ to 39.06. The overall Sr and Pb isotopic compositions of the igneous rocks indicate a generally moderate crustal assimilation of ancient radiogenic rocks. The Pb isotopic composition of sulfides from 14 polymetallic ore deposits in the study area lie on parallel arrays between the Pb isotopic compositions of spatially related igneous rocks and higher $$^{208}\mathrm{Pb}\,/ {}^{204}\mathrm{Pb}\,$$ and $$^{207}\mathrm{Pb}\,/ {}^{204}\mathrm{Pb}\,$$ sources such as Paleozoic and Mesozoic siliciclastic sedimentary rocks or the Carboniferous and older crystalline basement. The trace element and radiogenic isotope signature of igneous rocks related to mineralization indicates that these rocks have undergone limited midcrustal and shallow crustal assimilation and reflect melt equilibration in the lower crust at a crustal thickness of more than 40–45 km under conditions where hornblende and garnet were stable in the basaltic lower crustal residuum. Mineralization was favored by a change from normal to flat subduction, resulting in crustal thickening as well as broadening and subsequent cessation of the magmatic arc. However, some igneous rocks apparently unrelated to mineralization have high Sm/Yb and Sr/Y ratios as well. Petrographic and Pb isotopic evidence indicates that for some of these rocks, these trace element ratios may be better explained by shallow crustal hornblende fractionation or assimilation of pelitic material.

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 categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.011
Threshold uncertainty score0.972

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

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 head0.019
GPT teacher head0.204
Teacher spread0.186 · 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

Citations21
Published2009
Admission routes1
Has abstractyes

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