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Coesite in clinopyroxene in the Caledonides and its implications for geodynamics
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“Ultrahigh-pressure (UHP) metamorphism is defined in silicabearing rocks by the stabilization of coesite (Chopin, 1984;Smith, 1984) a high-pressure polymorph of quartzwhich occurs at ~90-100 km depth below the Earth's surface, assuming lithostatic pressure”
From Secular change and the onset of plate tectonics on Earth (2020) · cites this paper as Smith, 1984
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Zhang, Q., Gao, X., Chen, R., & Zheng, Y. (2023) · Science China Earth Sciences · doi:10.1007/s11430-023-1209-6 · Cited by 12
Hidden intact coesite in deeply subducted rocks
Taguchi, T., Kouketsu, Y., Igami, Y., Kobayashi, T., & Miyake, A. (2021) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2021.116763 · Cited by 12
Metadata
- Authors
- Smith, D. C.
- Affiliations
- Centre National de la Recherche Scientifique (FR)
- Corresponding author
- Smith, David C.
- ORCID
- Smith, David C.
- Venue
- Nature
- Published
- 1984-08
- Volume
- 310
- Issue
- 5979
- Pages
- 641-644
- ISSN
- 0028-0836 (ISSN-L)
- 1476-4687
- OpenAlex
- W1981344517
- Cited by
- 773
- References
- 15
- Citations by year
- 2026: 9 · 2025: 16 · 2024: 14 · 2023: 18 · 2022: 21 · 2021: 27 · 2020: 30 · 2019: 48 · 2018: 44 · 2017: 30 · 2016: 16 · 2015: 40 · 2014: 20 · 2013: 24 · 2012: 23
- FWCI
- 3.67
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.springer.com/tdm (tdm)
- Locations
- Nature (publishedVersion)
- 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 › Geology › Geological Studies and Exploration
- Keywords
- coesite, clinopyroxene, high-pressure metamorphism, subduction, obduction, geodynamics
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