Mantle geochemistry: The message from oceanic volcanism
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Discrete geochemical domains are thought to have persisted over hundred-million or billion-year timescales in the lower mantle, indicating that it is not as well mixed.
“Nonetheless, discrete geochemical domains are thought to have persisted over hundred-million or billion-year timescales in the lower mantle (Hofmann, 1997), indicating that it is not as well mixed.”
From Secular change and the onset of plate tectonics on Earth (2020) · cites this paper as Hofmann, 1997
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Production and recycling of oceanic crust in the early Earth
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The evolution of the 87sr/86sr of marine carbonates does not constrain continental growth
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- Authors
- Hofmann, A. W.
- Affiliations
- Max Planck Institute for Chemistry (DE)
- Corresponding author
- Hofmann, A. W.
- ORCID
- Hofmann, A. W.
- Venue
- Nature
- Published
- 1997-01
- Volume
- 385
- Issue
- 6613
- Pages
- 219-229
- ISSN
- 0028-0836 (ISSN-L)
- 1476-4687
- OpenAlex
- W1974731988
- Cited by
- 2,782
- References
- 116
- Citations by year
- 2026: 112 · 2025: 149 · 2024: 111 · 2023: 112 · 2022: 141 · 2021: 140 · 2020: 124 · 2019: 140 · 2018: 116 · 2017: 122 · 2016: 108 · 2015: 116 · 2014: 106 · 2013: 99 · 2012: 95
- FWCI
- 49.78
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.springer.com/tdm (tdm)
- Locations
- Nature (publishedVersion)
- RePEc: Research Papers in Economics (submittedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Astro and Planetary Science
- Physical Sciences › Earth and Planetary Sciences › Geophysics › High-pressure geophysics and materials
- Keywords
- mantle geochemistry, oceanic basalts, mantle heterogeneity, solid-state convection, trace element depletion, isotopic composition, mantle recycling, subduction, continental crust contamination, mantle evolution
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