On ultrahigh-temperature crustal metamorphism

Kelsey, David E.

doi:10.1016/j.gr.2007.06.001

Cited by 365Geological and Geochemical AnalysisHigh-pressure geophysics and materialsAstro and Planetary Science

On ultrahigh-temperature crustal metamorphism

Kelsey, David E.·2008·Gondwana Research

DOI 10.1016/j.gr.2007.06.001

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UHT metamorphism is rare in the Archean, being mostly associated with Proterozoic supercontinent accretion events, which themselves record evidence of horizontal plate motion.
“By contrast with normal granulites, UHT metamorphism is rare in the Archean, being mostly associated with Proterozoic supercontinent accretion events (e.g.Santosh et al., 2006;Kelsey, 2008;Li et al., 2019), which themselves record evidence of horizontal plate motion”
From Secular change and the onset of plate tectonics on Earth (2020) · cites this paper as Kelsey, 2008

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Authors: Kelsey, D. E.
Affiliations: The University of Adelaide (AU)
Corresponding author: Kelsey, David E.
Venue: Gondwana Research
Publisher: Elsevier BV
Published: 2008-01
Volume: 13
Issue: 1
Pages: 1-29
ISSN: 1342-937X (ISSN-L)
DOI: 10.1016/j.gr.2007.06.001
OpenAlex: W2000326123
Cited by: 365
References: 345
Citations by year: 2026: 11 · 2025: 9 · 2024: 24 · 2023: 13 · 2022: 15 · 2021: 25 · 2020: 23 · 2019: 20 · 2018: 21 · 2017: 20 · 2016: 21 · 2015: 19 · 2014: 30 · 2013: 19 · 2012: 21
FWCI: 17.46
Type: journal article
Language: en
Open access: closed
Licence: www.elsevier.com/tdm/userlicense/1.0/ (tdm)
Locations: Gondwana Research (publishedVersion)
Adelaide Research & Scholarship (AR&S) (University of Adelaide) (submittedVersion)
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: ultrahigh-temperature metamorphism, crustal metamorphism, mineral assemblages, pressure-temperature conditions, phase equilibria, deep crust, accretionary orogens, collisional orogens, lithospheric rheology, crust-mantle interaction, granulite facies metamorphism

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