Cooling of the Earth in the Archaean: Consequences of pressure-release melting in a hotter mantle
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Trace-element systematics of Archean sediments imply that oceanic plateaux were much more common than on modern-day Earth, and had equilibrium thicknesses of ~40-45 km.
“Trace-element systematics of Archean sediments imply that oceanic plateaux were much more common than on the modern-day Earth (Kamber, 2010), and had equilibrium thicknesses of ~40-45 km”
From Secular change and the onset of plate tectonics on Earth (2020) · cites this paper as Vlaar et al., 1994
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“Trace-element systematics of Archean sediments imply that oceanic plateaux were much more common than on the modern-day Earth (Kamber, 2010), and had equilibrium thicknesses of ~40–45 km (Vlaar et al., 1994; Korenaga, 2006).”
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- Authors
- Vlaar, N. J., van Keken, P. E., & van den Berg, A. P.
- Affiliations
- Utrecht University (NL)
- Venue
- Earth and Planetary Science Letters
- Publisher
- Elsevier BV
- Published
- 1994-01
- Volume
- 121
- Issue
- 1-2
- Pages
- 1-18
- ISSN
- 0012-821X (ISSN-L)
- OpenAlex
- W2121772518
- Cited by
- 128
- References
- 60
- Citations by year
- 2026: 1 · 2025: 3 · 2024: 3 · 2023: 1 · 2022: 2 · 2021: 2 · 2020: 3 · 2019: 4 · 2018: 3 · 2017: 8 · 2016: 5 · 2015: 6 · 2014: 2 · 2013: 10 · 2012: 8
- FWCI
- 2.84
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Earth and Planetary Science Letters (publishedVersion)
- 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 cooling, komatiite, greenstone belts, eclogite, continental roots, crustal root, mantle temperature, plate tectonics, magma migration, latent heat release, harzburgite
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