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 accessIntegrity signals
Registry
Cites
Statistics
Claims the paper makes
Claims other papers make about this one
Each is checked against this paper’s own text: does it say what the citing paper says it does?
Harlov (2000) identified CO2-rich fluids as the principal driver for oxidation of granulites from the Sveconorwegian Bamble terrane, which were metamorphosed during the Arendal phase around 1.14-1.08 GPa.
“For instance, Harlov (2000) identified CO 2rich fluids as the principal driver for oxidation of granulites from the Sveconorwegian Bamble terrane, which were metamorphosed during the Arendal phase around 1.14-1.08GPa (e.g., Bingen 2008).”
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 Harlov (2000)
Oxygen fugacity of metamorphic rocks plays a major role with respect to the Fe content and stability of silicate minerals and oxide phases.
“Oxygen fugacity of metamorphic rocks plays a major role with respect to the Fe content and stability of silicate minerals and oxides phases (e.g., Harlov 2000).”
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 Harlov 2000
Cited by
Sorted by citations
Duesterhoeft, E., Raase, P., Duguet, M., & Easton, R. M. (2021) · Canadian Journal of Earth Sciences · doi:10.1139/cjes-2019-0238 · Cited by 4 · see citing works
- Authors
- Harlov, D. E.
- Affiliations
- GFZ Helmholtz Centre for Geosciences (DE)
- Corresponding author
- Harlov, Daniel E.
- ORCID
- 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
- Licence
- 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
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
Are you an author, or do you see a problem with this page? Request a review