Precambrian geodynamics: Concepts and models
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Such a tectonic scenario, which is readily reproduced in two- and three-dimensional thermo-mechanical models of the Archean Earth, is supported in the geological record by the paucity of eclogites and refractory cumulate material.
“Such a tectonic scenario, which is readily reproduced in two-and threedimensional thermo-mechanical models of the Archean Earth (Gerya, 2014;Sizova et al., 2015;Fischer and Gerya, 2016a;Piccolo et al., 2019), is supported in the geological record by the paucity of eclogites and refractory cumulate material (see Sections 3.1 and 4.3).”
From Secular change and the onset of plate tectonics on Earth (2020) · cites this paper as Gerya, 2014
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“Such a tectonic scenario, which is readily reproduced in two- and threedimensional thermo-mechanical models of the Archean Earth (Gerya, 2014; Sizova et al., 2015; Fischer and Gerya, 2016a; Piccolo et al., 2019), is supported in the geological record by the paucity of eclogites and refractory…”
BackgroundInfluentialContrasting styles of Phanerozoic and Precambrian continental collision
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- Authors
- Gerya, T.
- Affiliations
- ETH Zurich (CH)
- Corresponding author
- Gerya, Taras
- ORCID
- Gerya, Taras
- Venue
- Gondwana Research
- Publisher
- Elsevier BV
- Published
- 2014-03
- Volume
- 25
- Issue
- 2
- Pages
- 442-463
- ISSN
- 1342-937X (ISSN-L)
- OpenAlex
- W2039669657
- Cited by
- 352
- References
- 115
- Citations by year
- 2026: 21 · 2025: 20 · 2024: 23 · 2023: 27 · 2022: 35 · 2021: 25 · 2020: 35 · 2019: 59 · 2018: 18 · 2017: 25 · 2016: 22 · 2015: 11 · 2014: 16 · 2013: 15
- FWCI
- 23.49
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Gondwana Research (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Geology › Geological and Geophysical Studies
- Physical Sciences › Earth and Planetary Sciences › Geophysics › High-pressure geophysics and materials
- Keywords
- plate tectonics, subduction initiation, plume tectonics, lithospheric delamination, mantle downwelling, gravitational tectonics, accretionary orogens, slab break-off, ultrahigh-pressure metamorphism, craton formation, craton stability, mantle temperature, lithospheric rheology
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