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Temperatures of serpentinization of ultramafic rocks based on O18/O16 fractionation between coexisting serpentine and magnetite

Wenner, David B., Taylor, Hugh P.·1971·Contributions to Mineralogy and Petrology

DOI 10.1007/bf00643332

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Authors: Wenner, D. B., & Taylor, H. P.
Affiliations: California Institute of Technology (US)
Venue: Contributions to Mineralogy and Petrology
Publisher: Springer Science and Business Media LLC
Published: 1971-09
Volume: 32
Issue: 3
Pages: 165-185
ISSN: 0010-7999 (ISSN-L)
1432-0967
DOI: 10.1007/bf00643332
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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Temperatures of serpentinization of ultramafic rocks based on O18/O16 fractionation between coexisting serpentine and magnetite

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