Reaction enhanced permeability during retrogressive metamorphism
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Complete carbon mineralization of peridotite may result from positive feedback in which reaction-driven volume changes cause increases in differential stress and generate fractures, maintaining or increasing permeability and exposing fresh reactive surfaces.
“This may be the result of positive feedback, in which reaction-driven volume changes cause increases in differential stress in the rock and generate fractures, maintaining or increasing the permeability of the rock and exposing fresh reactive surfaces”
From An Overview of the Status and Challenges of CO2 Storage in Minerals and Geological Formations (2019) · cites this paper as Jamtveit et al., 2008
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In situ carbonation of peridotite for CO <sub>2</sub> storage
Kelemen, P. B., & Matter, J. (2008) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.0805794105 · Cited by 750 · see citing works
An Overview of the Status and Challenges of CO2 Storage in Minerals and Geological Formations
Kelemen, P., Benson, S. M., Pilorgé, H., Psarras, P., & Wilcox, J. (2019) · Frontiers in Climate · doi:10.3389/fclim.2019.00009 · Cited by 587 · see citing works
Kelemen, P. B., Matter, J., Streit, E. E., Rudge, J. F., Curry, W. B., & Blusztajn, J. (2011) · Annual Review of Earth and Planetary Sciences · doi:10.1146/annurev-earth-092010-152509 · Cited by 518 · see citing works
Rudge, J. F., Kelemen, P. B., & Spiegelman, M. (2010) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2010.01.016 · Cited by 166 · see citing works
Microstructure and porosity evolution during experimental carbonation of a natural peridotite
Hövelmann, J., Austrheim, H., & Jamtveit, B. (2012) · Chemical Geology · doi:10.1016/j.chemgeo.2012.10.025 · Cited by 139 · see citing works
Self-citationNanoscale constraints on porosity generation and fluid flow during serpentinization
Tutolo, B. M., Mildner, D. F. R., Gagnon, C. V. L., Saar, M. O., & Seyfried, W. E. (2016) · Geology · doi:10.1130/g37349.1 · Cited by 94 · see citing works
- Authors
- Jamtveit, B., Malthe-Sørenssen, A., & Kostenko, O.
- Affiliations
- University of Oslo (NO)
- Shell (United States) (US)
- Corresponding author
- Jamtveit, Bjørn
- ORCID
- Jamtveit, Bjørn
- Venue
- Earth and Planetary Science Letters
- Publisher
- Elsevier BV
- Published
- 2008-03
- Volume
- 267
- Issue
- 3-4
- Pages
- 620-627
- ISSN
- 0012-821X (ISSN-L)
- OpenAlex
- W1989885750
- Cited by
- 140
- References
- 0
- Citations by year
- 2026: 11 · 2025: 12 · 2024: 9 · 2023: 6 · 2022: 2 · 2021: 9 · 2020: 9 · 2019: 9 · 2018: 10 · 2017: 10 · 2016: 9 · 2015: 5 · 2014: 6 · 2013: 6 · 2012: 10
- FWCI
- 3.37
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- Locations
- Earth and Planetary Science Letters (publishedVersion)
- Funders
- Norges Forskningsråd
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Physical Sciences › Engineering › Mechanics of Materials › Rock Mechanics and Modeling
- Physical Sciences › Earth and Planetary Sciences › Geophysics › High-pressure geophysics and materials
- Keywords
- retrograde metamorphism, fluid migration, permeability, olivine hydration, serpentinization, troctolite, microfracture, dilatancy, spring network model, porosity generation, stress heterogeneity, Duluth Complex, metamorphic reactions
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
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