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Temperatures of serpentinization of ultramafic rocks based on O18/O16 fractionation between coexisting serpentine and magnetite
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“These temperatures are lower than typical serpentinization temperatures in continental settings (85-115 ° C in chrysotile-lizardite mineralogies; Wenner and Taylor, 1971), in agreement with the observation that magnesite vein mineralization postdates serpentinization in the host peridotite rock.”
From Clumped-isotope thermometry of magnesium carbonates in ultramafic rocks (2016) · cites this paper as Wenner and Taylor, 1971
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Metadata
- Authors
- Wenner, D. B., & Taylor, H. P.
- Affiliations
- California Institute of Technology (US)
- Venue
- Contributions to Mineralogy and Petrology
- Published
- 1971-09
- Volume
- 32
- Issue
- 3
- Pages
- 165-185
- ISSN
- 0010-7999 (ISSN-L)
- 1432-0967
- OpenAlex
- W1988978036
- Cited by
- 405
- References
- 33
- Citations by year
- 2026: 9 · 2025: 8 · 2024: 8 · 2023: 11 · 2022: 7 · 2021: 7 · 2020: 7 · 2019: 13 · 2018: 9 · 2017: 8 · 2016: 7 · 2015: 13 · 2014: 16 · 2013: 9 · 2012: 9
- FWCI
- 4.12
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.springer.com/tdm (tdm)
- Locations
- Contributions to Mineralogy and Petrology (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Keywords
- serpentinization, ultramafic rocks, oxygen isotope fractionation, antigorite, lizardite, chrysotile, chlorite, Mid-Atlantic Ridge
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