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The continental lithosphere–asthenosphere boundary: Can we sample it?
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“These different modes and length scales of heat transfer cause Archean and Proterozoic lithosphere to exhibit distinctly different geochemical and isotopic signatures to the underlying asthenosphere, which may compositionally homogenize over geological time”
From Secular change and the onset of plate tectonics on Earth (2020) · cites this paper as O'Reilly and Griffin, 2010
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Metadata
- Authors
- O'Reilly, S. Y., & Griffin, W. L.
- Affiliations
- Macquarie University (AU)
- Corresponding author
- O'Reilly, Suzanne Y.
- Venue
- Lithos
- Publisher
- Elsevier BV
- Published
- 2010-11
- Volume
- 120
- Issue
- 1-2
- Pages
- 1-13
- ISSN
- 0024-4937 (ISSN-L)
- OpenAlex
- W2000509346
- Cited by
- 162
- References
- 131
- Citations by year
- 2026: 9 · 2025: 6 · 2024: 13 · 2023: 7 · 2022: 9 · 2021: 17 · 2020: 16 · 2019: 16 · 2018: 7 · 2017: 7 · 2016: 13 · 2015: 6 · 2014: 18 · 2013: 3 · 2012: 7
- FWCI
- 4.95
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Lithos (publishedVersion)
- Funders
- Macquarie University
- Australian Research Council
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Geophysics › High-pressure geophysics and materials
- Physical Sciences › Earth and Planetary Sciences › Space and Planetary Science › Astro and Planetary Science
- Keywords
- lithosphere-asthenosphere boundary, lithospheric mantle, asthenosphere, metasomatism, eclogite, peridotite xenoliths, Re-Os isotopes, diamond inclusions, cratons, lithospheric delamination, mantle plume, lithospheric extension, mantle upwelling
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