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The contribution of metamorphic petrology to understanding lithosphere evolution and geodynamics
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Mantle temperatures at 1.0 Ga are inferred to have been >100°C warmer than present.
“mantle temperatures at 1.0 Ga are inferred to have been >100 o C warmer than present(Brown 2014)”
From The Grenville Province: revisiting the orogenic framework and integrating recent findings (2025) · cites this paper as Brown 2014
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Thermal history of the Earth and its petrological expression
Herzberg, C., Condie, K., & Korenaga, J. (2010) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2010.01.022 · Cited by 1,148 · cited 7×
“D numerical experiments of oceanic subduction that demonstrate a change to one-sided subduction is plausible as upper mantle temperature declined to 200 C warmer than at present during the late NeoarcheanePaleoproterozoic.”
BackgroundInfluentialA change in the geodynamics of continental growth 3 billion years ago
Dhuime, B., Hawkesworth, C. J., Cawood, P. A., & Storey, C. D. (2012) · Science · doi:10.1126/science.1216066 · Cited by 923
Moyen, J.-F. (2011) · Lithos · doi:10.1016/j.lithos.2010.09.015 · Cited by 708
Blueschists and eclogites of the world and their exhumation
Maruyama, S., Liou, J. G., & Terabayashi, M. (1996) · International Geology Review · doi:10.1080/00206819709465347 · Cited by 625
Stern, R. J. (2005) · Geology · doi:10.1130/g21365.1 · Cited by 582
Initiation and evolution of plate tectonics on Earth: Theories and observations
Korenaga, J. (2013) · Annual Review of Earth and Planetary Sciences · doi:10.1146/annurev-earth-050212-124208 · Cited by 533
Precambrian geodynamics: Concepts and models
Gerya, T. (2014) · Gondwana Research · doi:10.1016/j.gr.2012.11.008 · Cited by 352
Stagnant-lid tectonics in early Earth revealed by 142Nd variations in late Archean rocks
Debaille, V., O'Neill, C., Brandon, A. D., Haenecour, P., Yin, Q.-Z., Mattielli, N., & Treiman, A. H. (2013) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2013.04.016 · Cited by 230 · cited 2×
“For example, a strong case has been made for a stagnant-lid plate tectonics regime on the early Earth (Debaille et al., 2013; Griffin et al., 2013; O’Neill et al., 2013; hereafter “stagnant lid”).”
BackgroundMetamorphism and melting of picritic crust in the early Earth
Ziaja, K., Foley, S. F., White, R. W., & Buhre, S. (2014) · Lithos · doi:10.1016/j.lithos.2013.07.001 · Cited by 34
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Metadata
- Authors
- Brown, M.
- Venue
- Geoscience Frontiers
- Publisher
- Elsevier BV
- Published
- 2014-07
- Volume
- 5
- Issue
- 4
- Pages
- 553-569
- ISSN
- 1674-9871
- Cited by
- 279
- References
- 9
- Language
- en
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