Bibliographic record
Abstract
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.
How this classification was reachedexpand
Full frame machine prediction
Teacher imitationNot calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.
Distilled classifier scores by category (both heads)
| Category | Codex | Gemma |
|---|---|---|
| Metaresearch | 0.001 | 0.003 |
| Meta-epidemiology (narrow) | 0.001 | 0.000 |
| Meta-epidemiology (broad) | 0.001 | 0.000 |
| Bibliometrics | 0.002 | 0.002 |
| Science and technology studies | 0.004 | 0.004 |
| Scholarly communication | 0.007 | 0.007 |
| Open science | 0.001 | 0.002 |
| Research integrity | 0.002 | 0.002 |
| Insufficient payload (model declined to judge) | 0.055 | 0.015 |
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.
score_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from itClassification
machine, unvalidatedMachine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.
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".