Lizardite versus antigorite serpentinite: magnetite, hydrogen, and life (?)
Abstract
Research Article| October 01, 2010 Lizardite versus antigorite serpentinite: Magnetite, hydrogen, and life(?) Bernard W. Evans Bernard W. Evans Department of Earth and Space Sciences, Box 351310, University of Washington, Seattle, Washington 98195-1310, USA Search for other works by this author on: GSW Google Scholar Geology (2010) 38 (10): 879–882. https://doi.org/10.1130/G31158.1 Article history received: 26 Feb 2010 rev-recd: 30 Apr 2010 accepted: 04 May 2010 first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Bernard W. Evans; Lizardite versus antigorite serpentinite: Magnetite, hydrogen, and life(?). Geology 2010;; 38 (10): 879–882. doi: https://doi.org/10.1130/G31158.1 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 SocietyGeology Search Advanced Search Abstract The serpentinization of peridotite operates according to one or the other, or a combination, of two end-member mechanisms. In low-temperature environments (50–300 °C), where lizardite is the predominant serpentine mineral, olivine is consumed by reaction with H2O but its composition (Mg#) remains unchanged. Mg-rich lizardite, magnetite, and dihydrogen gas (±brucite) are products of the reaction. At higher temper…
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Carbonate mineralization in obducted segments of serpentinized peridotite and serpentinite occurs at temperatures at or lower than serpentinization temperatures (50-300 °C).
“and, by inference, occurs at temperatures at or lower than serpentinization temperatures (50-300 ° C; Evans, 2010).”
From Clumped-isotope thermometry of magnesium carbonates in ultramafic rocks (2016) · cites this paper as Evans, 2010
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- Authors
- Evans, B. W.
- Affiliations
- University of Washington (US)
- Corresponding author
- Evans, Bernard W.
- Venue
- Geology
- Publisher
- Geological Society of America
- Published
- 2010-10
- Volume
- 38
- Issue
- 10
- Pages
- 879-882
- ISSN
- 0091-7613 (ISSN-L)
- 1943-2682
- OpenAlex
- W2323944982
- Cited by
- 229
- References
- 4
- Citations by year
- 2026: 16 · 2025: 16 · 2024: 14 · 2023: 17 · 2022: 12 · 2021: 17 · 2020: 20 · 2019: 13 · 2018: 8 · 2017: 22 · 2016: 17 · 2015: 6 · 2014: 13 · 2013: 11 · 2012: 11
- FWCI
- 6.61
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Geology (publishedVersion)
- Topics
- Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Origins and Evolution of Life
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Keywords
- lizardite, antigorite, serpentinization, peridotite, magnetite, molecular hydrogen, olivine, brucite, forearc mantle wedge, serpentine minerals, olivine composition
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