Comparison of garnet-biotite, calcite-graphite, and calcite-dolomite thermometry in the Grenville Orogen; Ontario, Canada
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The Grt-Bt temperature of 670°C and GASP pressure of 0.6 GPa for sample BAN015 is identical with temperatures of 650 °C and 670 °C (and GASP pressure of 0.53 GPa) found in the same area by Rathmell et al. (1999) and Dunn (2005), respectively.
“This temperature is identical with the Grt-Bt geothermometer temperature of 650 °C and 670 °C (and GASP pressure of 0.53 GPa) found in the same area by Rathmell et al. (1999) and Dunn (2005), respectively.”
From The role of excess oxygen for modeling high-Mn, low-Ca garnets in metapelites from the northern Central Metasedimentary Belt of the Grenville Province, Ontario, Canada (2021) · cites this paper as Rathmell et al. (1999)
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References 35 · Cited by 29
- Authors
- Rathmell, M. A., Streepey, M. M., Essene, E. J., & van der Pluijm, B. A.
- Affiliations
- University of Michigan (US)
- Venue
- Contributions to Mineralogy and Petrology
- Published
- 1999-02
- Volume
- 134
- Issue
- 2-3
- Pages
- 217-231
- ISSN
- 0010-7999 (ISSN-L)
- 1432-0967
- OpenAlex
- W2169035735
- Cited by
- 29
- References
- 35
- Citations by year
- 2025: 1 · 2023: 1 · 2022: 2 · 2019: 1 · 2018: 2 · 2017: 2 · 2013: 1
- FWCI
- 0.67
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.springer.com/tdm (tdm)
- Locations
- Contributions to Mineralogy and Petrology (publishedVersion)
- Deep Blue (University of Michigan) (acceptedVersion)
- Funders
- National Science Foundation
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Geology › Geological Studies and Exploration
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Keywords
- garnet-biotite thermometry, Grenville orogen, regional metamorphism, peak metamorphic temperature, isograds, retrogression, metapelites, Madoc, Bancroft
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