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Record W2317917382 · doi:10.2113/gselements.9.2.99

Serpentinite: What, Why, Where?

2013· article· en· W2317917382 on OpenAlex

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.

affAt least one author lists a Canadian institution in the pinned OpenAlex snapshot.

Bibliographic record

VenueElements · 2013
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsUniversity of Ottawa
Fundersnot available
KeywordsCitationLibrary scienceArt historyArtComputer science

Abstract

fetched live from OpenAlex

Research Article| April 01, 2013 Serpentinite: What, Why, Where? Bernard W. Evans; Bernard W. Evans 1Department of Earth and Space Sciences, University of Washington, Seattle, WA 98195-1310, USAE-mail: bwevans@u.washington.edu Search for other works by this author on: GSW Google Scholar Keiko Hattori; Keiko Hattori 2Department of Earth Sciences, University of OttawaOttawa, ON K1N 6N5, CanadaE-mail: khattori@uottawa.ca Search for other works by this author on: GSW Google Scholar Alain Baronnet Alain Baronnet 3Centre Interdisciplinaire de Nanosciences de Marseille, CNRS, Aix-Marseille Université, 13288, Marseille, FranceE-mail: baronnet@cinam.univ-mrs.fr Search for other works by this author on: GSW Google Scholar Author and Article Information Bernard W. Evans 1Department of Earth and Space Sciences, University of Washington, Seattle, WA 98195-1310, USAE-mail: bwevans@u.washington.edu Keiko Hattori 2Department of Earth Sciences, University of OttawaOttawa, ON K1N 6N5, CanadaE-mail: khattori@uottawa.ca Alain Baronnet 3Centre Interdisciplinaire de Nanosciences de Marseille, CNRS, Aix-Marseille Université, 13288, Marseille, FranceE-mail: baronnet@cinam.univ-mrs.fr Publisher: Mineralogical Society of America First Online: 09 Mar 2017 Online ISSN: 1811-5217 Print ISSN: 1811-5209 © 2013 by the Mineralogical Society of America Elements (2013) 9 (2): 99–106. https://doi.org/10.2113/gselements.9.2.99 Article history First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Bernard W. Evans, Keiko Hattori, Alain Baronnet; Serpentinite: What, Why, Where?. Elements 2013;; 9 (2): 99–106. doi: https://doi.org/10.2113/gselements.9.2.99 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyElements Search Advanced Search Abstract Rock-forming serpentine minerals form flat, cylindrical, and corrugated crystal microstructures, which reflect energetically efficient layering of alternate tetrahedral and octahedral sheets. Serpentinization of peridotite involves internal buffering of the pore fluid, reduction of oxygen fugacity, and partial oxidation of Fe2+ to Fe3+. Sluggish MgFe diffusion in olivine causes precipitation of magnetite and release of H2. The tectonic environment of the serpentinization process dictates the abundance of fluid-mobile elements in serpentinites. Similar enrichment patterns of fluid-mobile elements in mantle-wedge serpentinites and arc magmas suggest a linkage between the dehydration of serpentinite and arc magmatism. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

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)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesInsufficient payload (model declined to judge)
Consensus categoriesInsufficient payload (model declined to judge)
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.294
Threshold uncertainty score0.989

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 studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.3060.012

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 head0.010
GPT teacher head0.193
Teacher spread0.183 · 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