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Record W2163583859 · doi:10.1093/petrology/41.1.43

‘Subduction Style’ Magmatism in a Non-subduction Setting: the Colville Igneous Complex, NE Washington State, USA

2000· article· en· W2163583859 on OpenAlex
G. A. Morris, Peter B. Larson, P. R. Hooper

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

aboutThe title or abstract carries a Canadian signal from the geographic lexicon.
no affNo Canadian affiliation: this work is invisible to an affiliation-only frame.
No Canadian affiliation. An affiliation-only frame, the usual design, would never have seen this work. It is one of the works that make the case for inverting the frame.

Bibliographic record

VenueJournal of Petrology · 2000
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsnot available
Fundersnot available
KeywordsGeologyAndesitesGeochemistryIgneous rockBasaltMagmatismLileSubductionPetrogenesisPartial meltingLarge igneous provinceVolcanic rockAndesiteVolcanoPaleontologyTectonics

Abstract

fetched live from OpenAlex

The Colville Igneous Complex is located within the Eocene Magmatic Belt of the North American Cordilleran interior. It straddles the US–Canadian border in northeast Washington and southern British Columbia. The complex consists of three intrusive and two extrusive phases, the first extrusive phase being contemporaneous with the latter two intrusive phases. As a consequence of sub-solidus re-equilibration in the plutonic rocks, this study concentrates on the two extrusive phases, the Sanpoil Volcanic Formation and the Klondike Mountain Formation. The Sanpoil Volcanic Formation consists of andesites, dacites and rare trachyandesites (SiO2 = 55–70 wt %) exhibiting a slight decrease in total alkalis (Na2O + K2O) with increasing silica. The Klondike Mountain Formation consists of basalts, basaltic andesites, andesites, dacites and rhyolites (SiO2 = 51–75 wt %) with total alkalis increasing with increasing silica. The calc-alkaline affinity of the rocks of the Colville Igneous Complex, coupled with the presence of a 'subduction signature' of enriched large ion lithophile elements (LILE) and depleted high field strength elements (HFSE), has traditionally been attributed to petrogenesis in a subduction-related magmatic arc, the 'Challis Arc'. New trace and rare earth element and isotopic data (87Sr/86Sri, ϵNdi, δ18O), however, suggest that this explanation is no longer tenable. We propose that the magmas of the Sanpoil Volcanic Formation were generated by mid-crustal partial melting of a mid-Proterozoic source and that the Klondike Mountain Formation was formed by varying degrees of mixing between two distinct late-Proterozoic lower-crustal sourced magmas and a mantle-derived magma. In all cases, the subduction or calc-alkaline signature was inherited from the Proterozoic crustal sources. The only magmas that can confidently be attributed to a mantle source are the basalts of the Klondike Mountain Formation, which show no decoupling of the LILE and HFSE, i.e. no subduction signature, precluding the presence of a subduction slab beneath this part of the North American Cordillera during the Eocene. We propose the alternative model: that the Colville Igneous Complex formed as a result of decompression melting of crust and mantle during post-Laramide orogenic collapse of an overthickened crust.

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.

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 score0.324
Threshold uncertainty score0.985

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)0.0160.000

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 head0.008
GPT teacher head0.202
Teacher spread0.194 · 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