Cited by 46Geological and Geochemical AnalysisGeochemistry and Elemental AnalysisAstro and Planetary Science

Titaniferous magnetite–ilmenite thermometry and titaniferous magnetite–ilmenite–orthopyroxene–quartz oxygen barometry in granulite facies gneisses, Bamble Sector, SE Norway: implications for the role of high-grade CO2-rich fluids during granulite genesis

Open access
Harlov, Daniel E.·2000·Contributions to Mineralogy and Petrology

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Crossref · 10.1007/pl00007670

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Authors
Harlov, D. E.
Affiliations
GFZ Helmholtz Centre for Geosciences (DE)
Corresponding author
Harlov, Daniel E.
Venue
Contributions to Mineralogy and Petrology
Published
2000-06-06
Volume
139
Issue
2
Pages
180-197
ISSN
0010-7999 (ISSN-L)
OpenAlex
W2049012462
Cited by
46
References
0
Citations by year
2026: 3 · 2024: 2 · 2023: 1 · 2022: 2 · 2021: 3 · 2020: 2 · 2019: 6 · 2018: 1 · 2017: 1 · 2016: 3 · 2015: 1 · 2014: 3 · 2012: 2
FWCI
0.85
Type
journal article
Language
en
Open access
Locations
  • Contributions to Mineralogy and Petrology (publishedVersion)
  • Publication Database GFZ (GFZ German Research Centre for Geosciences) (submittedVersion)
  • Publication Database GFZ (GFZ German Research Centre for Geosciences) (submittedVersion, cc-by)
Funders
  • National Science Foundation
  • Purdue University
Topics
  • Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
  • Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
  • Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Astro and Planetary Science
Keywords
oxygen fugacity, granulite facies gneiss, CO2-rich fluids, retrograde metamorphism

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