Genesis of magnesite deposits – models and trends
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Cryptocrystalline magnesite appears to be a widespread alteration product of dunite, peridotite, and serpentinite related to ophiolite bodies worldwide.
“Cryptocrystalline magnesite appears to be a widespread alteration product of dunite, peridotite, and serpentinite related to ophiolite bodies worldwide (Pohl, 1990; AbuJaber and Kimberley, 1992b; Schroll, 2002).”
From Clumped-isotope thermometry of magnesium carbonates in ultramafic rocks (2016) · cites this paper as Pohl, 1990
Field observations, structural relationships, and classical stable isotope thermometry of ultramafic-hosted cryptocrystalline magnesite have been applied to various extents, with relatively limited focus on hydrous magnesium carbonates.
“Field observations, structural relationships, and classical stable isotope thermometry of ultramafic-hosted cryptocrystalline magnesite have been applied to various extents (Petrov, 1980; Pohl, 1990; Jedrysek and Halas, 1990; Fallick et al., 1991; Abu-Jaber and Kimberley, 1992; Zedef et al., 2000; Ghoneim et al., 2003; Gartzos, 2004; Ece et al., 2005; Mirnejad et al., 2008; Jurkovic ´ et al., 2012”
From Clumped-isotope thermometry of magnesium carbonates in ultramafic rocks (2016) · cites this paper as Pohl, 1990
Genetic models for the formation of ultramafic-hosted cryptocrystalline magnesite proposed to date are varied and appear to be site-specific.
“Genetic models for the formation of ultramafic-hosted cryptocrystalline magnesite proposed to date are varied and appear to be site-specific (Petrov, 1980; Pohl, 1990; Jedrysek and Halas, 1990; Fallick et al., 1991; Abu-Jaber and Kimberley, 1992a; Zedef et al., 2000; Ghoneim et al., 2003; Gartzos, 2004; Ece et al., 2005; Kelemen and Matter, 2008; Mirnejad et al., 2008; Jurkovic ´ et al., 2012;”
From Clumped-isotope thermometry of magnesium carbonates in ultramafic rocks (2016) · cites this paper as Pohl, 1990
Most magnesite deposits do not occur in close relation to laterites.
“Although some magnesite deposits are clearly associated with laterite weathering zones (Quesnel et al., 2013), most magnesite deposits do not occur in close relation to laterites (Pohl, 1990).”
From Clumped-isotope thermometry of magnesium carbonates in ultramafic rocks (2016) · cites this paper as Pohl, 1990
Cites
O'Neil, J. R., & Barnes, I. (1971) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(71)90067-6 · Cited by 136 · see citing works
Aharon, P. (1988) · Chemical Geology · doi:10.1016/0009-2541(88)90164-7 · Cited by 89 · see citing works
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Clumped-isotope thermometry of magnesium carbonates in ultramafic rocks
García del Real, P., Maher, K., Kluge, T., Bird, D. K., Brown, G. E., & John, C. M. (2016) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2016.08.003 · Cited by 50 · see citing works
Azer, M. K., Gahlan, H. A., Asimow, P. D., Mubarak, H. S., & Al-Kahtany, K. M. (2019) · The Journal of Geology · doi:10.1086/700652 · Cited by 43 · see citing works
Hobbs, F. W. C., & Xu, H. (2020) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2019.10.014 · Cited by 41 · see citing works
- Authors
- Pohl, W.
- Affiliations
- Technische Universität Braunschweig (DE)
- Corresponding author
- Pohl, W.
- ORCID
- Pohl, W.
- Venue
- Geologische Rundschau
- Published
- 1990-06
- Volume
- 79
- Issue
- 2
- Pages
- 291-299
- ISSN
- 1437-3254 (ISSN-L)
- 0016-7835
- 1437-3262
- OpenAlex
- W2086247128
- Cited by
- 83
- References
- 2
- Citations by year
- 2026: 2 · 2025: 3 · 2024: 5 · 2023: 4 · 2022: 7 · 2021: 6 · 2020: 6 · 2019: 3 · 2018: 2 · 2017: 1 · 2016: 4 · 2015: 1 · 2014: 3 · 2013: 5 · 2012: 2
- FWCI
- 1.54
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.springer.com/tdm (tdm)
- Locations
- International Journal of Earth Sciences (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Earth-Surface Processes › Geological formations and processes
- Keywords
- magnesite deposits, diagenesis, evaporites, sabkha, hydrothermal replacement, supergene alteration, epithermal deposits, ultramafic rocks, genetic models, magnesium content
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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.
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