Geochemistry and petrology of listvenite in the Samail ophiolite, Sultanate of Oman: Complete carbonation of peridotite during ophiolite emplacement
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More recently investigated listvenite from Wadi Mansah is characterized by magnesite as the dominant carbonate mineral consistent with peridotite alteration predominately driven by influx of CO2.
“More recently investigated listvenite from Wadi Mansah is characterized by magnesite as the dominant carbonate mineral consistent with peridotite alteration predominately driven by influx of CO 2 (Falk & Kelemen, 2015).”
From Ultramafic Rock Carbonation: Constraints From Listvenite Core BT1B, Oman Drilling Project (2020) · cites this paper as Falk & Kelemen, 2015
Full carbonation of peridotites is possible at natural conditions of about 100°C.
“The presence of listvenites-fully carbonated peridotites composed entirely of magnesite and dolomite (MgCO 3 , CaMg(CO 3 ) 2 ) + quartz (SiO 2 ) + hematite and goethite (Fe 2 O 3 , FeO(OH)) + relict spinel and/or chromian mica-show that full carbonation of peridotites is possible at natural conditions (about 100 • C)”
From An Overview of the Status and Challenges of CO2 Storage in Minerals and Geological Formations (2019) · cites this paper as Falk and Kelemen, 2015
Geologic examples demonstrate that complete, in situ carbon mineralization of peridotite is possible at elevated temperature and relatively high partial pressures of CO2.
“Geologic examples demonstrate that complete, in situ carbon mineralization of peridotite is possible at elevated temperature and relatively high partial pressures of CO 2”
From An Overview of the Status and Challenges of CO2 Storage in Minerals and Geological Formations (2019) · cites this paper as Falk and Kelemen, 2015
Including the raw data of Falk and Kelemen (2015) (n=6) in the calculation yields an acid fractionation correction of 0.070 ± 0.033‰ (n=12), within error of the average from the samples analyzed here.
“Including the raw data of Falk and Kelemen (2015) ( n = 6) in the calculation of the acid-reaction yields a value of 0.070 ± 0.033 ‰ ( n =12), within error of the average from the samples analyzed here.”
From Clumped-isotope thermometry of magnesium carbonates in ultramafic rocks (2016) · cites this paper as Falk and Kelemen, 2015
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An Overview of the Status and Challenges of CO2 Storage in Minerals and Geological Formations
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Ultramafic Rock Carbonation: Constraints From Listvenite Core BT1B, Oman Drilling Project
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“The recently obtained 97 ± 29 Ma Rb‐Sr isochron age of listvenite fuchsite, and the fact that listvenites in the Samail ophiolite are only found along the basal thrust and associated mélange zones, are consistent with syn‐emplacement alteration of the ophiolite (Falk & Kelemen, 2015).”
BackgroundResultInfluentialSelf-citationIn situ carbon mineralization in ultramafic rocks: natural processes and possible engineered methods
Kelemen, P. B., Aines, R., Bennett, E., Benson, S. M., Carter, E., Coggon, J. A., de Obeso, J. C., Evans, O., Gadikota, G., Dipple, G. M., et al. (2018) · Energy Procedia · doi:10.1016/j.egypro.2018.07.013 · Cited by 74 · see citing works
Self-citationClumped-isotope thermometry of magnesium carbonates in ultramafic rocks
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Low temperature carbonation and CO2 mineral trapping in altered hydrotalcite-rich ultrmafic rocks
Leila, M., Hazlett, R., George, P.-M., Šegvić, B., & Fustic, M. (2025) · Scientific Reports · doi:10.1038/s41598-025-16025-1 · Cited by 16 · see citing works
“All reactions demonstrate the onset of precipitation of nesquehonite when the pH swings from acidic to alkaline implying that optimal nesquehonite precipitation occurs at pH values around 8.”
- Authors
- Falk, E. S., & Kelemen, P. B.
- Affiliations
- Lamont-Doherty Earth Observatory (US)
- Corresponding author
- Falk, Elisabeth S.
- Venue
- Geochimica et Cosmochimica Acta
- Publisher
- Elsevier BV
- Published
- 2015-07
- Volume
- 160
- Pages
- 70-90
- ISSN
- 0016-7037 (ISSN-L)
- OpenAlex
- W2069188138
- Cited by
- 189
- References
- 19
- Citations by year
- 2026: 18 · 2025: 23 · 2024: 14 · 2023: 19 · 2022: 27 · 2021: 29 · 2020: 18 · 2019: 14 · 2018: 11 · 2017: 8 · 2016: 7 · 2015: 1
- FWCI
- 8.69
- Type
- journal article
- Language
- en
- Open access
- bronze
- doi.org
- Licence
- Locations
- Geochimica et Cosmochimica Acta (acceptedVersion)
- OSTI OAI (U.S. Department of Energy Office of Scientific and Technical Information) (submittedVersion)
- Funders
- National Science Foundation (EAR-1049905)
- U.S. Department of Energy (DE-FE0002386, DGE-07-0742)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Physical Sciences › Environmental Science › Environmental Engineering › CO2 Sequestration and Geologic Interactions
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Keywords
- listvenite, Samail ophiolite, ophiolite emplacement, mantle wedge, carbon storage, CO2-rich fluids, clumped isotope thermometry, Rb-Sr isochron, metasedimentary rocks, serpentinized peridotite
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