Melting in an Archaean mantle plume: Heads it’s basalts, tails it’s komatiites
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Equivalent calculations for komatiitic basalts suggest liquidus temperatures of ~1650-1800 °C, consistent with independent experimental and field evidence that such high-MgO lavas form above mantle plumes.
“Equivalent calculations for komatiitic basalts suggest liquidus temperatures of ~1650-1800 °C, consistent with independent experimental and field evidence that such high-MgO lavas form above mantle plumes”
From Secular change and the onset of plate tectonics on Earth (2020) · cites this paper as Campbell et al., 1989
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- Authors
- Campbell, I. H., Griffiths, R. W., & Hill, R. I.
- Affiliations
- Australian National University (AU)
- Venue
- Nature
- Published
- 1989-06
- Volume
- 339
- Issue
- 6227
- Pages
- 697-699
- ISSN
- 0028-0836 (ISSN-L)
- 1476-4687
- OpenAlex
- W2030142526
- Cited by
- 470
- References
- 27
- Citations by year
- 2026: 8 · 2025: 6 · 2024: 24 · 2023: 8 · 2022: 13 · 2021: 19 · 2020: 12 · 2019: 14 · 2018: 11 · 2017: 15 · 2016: 12 · 2015: 18 · 2014: 11 · 2013: 17 · 2012: 22
- FWCI
- 10.27
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.springer.com/tdm (tdm)
- Locations
- Nature (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Geophysics › High-pressure geophysics and materials
- Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Astro and Planetary Science
- Keywords
- komatiite, basalt, mantle melting, greenstone belts, mantle thermal structure, mantle composition
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