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Osumilite-sapphirine-quartz granulites from Enderby Land, Antarctica: P-T conditions of metamorphism, implications for garnet-cordierite equilibria and the evolution of the deep crust
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Citations
Cited by
Vielzeuf, D., & Holloway, J. R. (1988) · Contributions to Mineralogy and Petrology · doi:10.1007/bf00375178 · Cited by 1,108
The origins of granulites: A metamorphic perspective
Harley, S. L. (1989) · Geological Magazine · doi:10.1017/s0016756800022330 · Cited by 1,042
TitaniQ: a titanium-in-quartz geothermometer
Wark, D. A., & Watson, E. B. (2006) · Contributions to Mineralogy and Petrology · doi:10.1007/s00410-006-0132-1 · Cited by 728
Pressure–temperature–time paths and a tectonic model for the evolution of granulites
Bohlen, S. R. (1987) · The Journal of Geology · doi:10.1086/629159 · Cited by 461
Kelsey, D. E., & Hand, M. (2015) · Geoscience Frontiers · doi:10.1016/j.gsf.2014.09.006 · Cited by 441
Metadata
- Authors
- Ellis, D. J.
- Venue
- Contributions to Mineralogy and Petrology
- Published
- 1980
- Volume
- 74
- Issue
- 2
- Pages
- 201-210
- ISSN
- 0010-7999 (ISSN-L)
- 1432-0967
- OpenAlex
- W2029370166
- Cited by
- 211
- References
- 0
- FWCI
- 3.80
- Type
- journal article
- Language
- en
- Open access
- closed
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.
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How to cite
Cite CoChat for the checks on this page, and the paper for its own findings.
- This page
- CoChat. (2026). Citation check: Osumilite-sapphirine-quartz granulites from Enderby Land, Antarctica: P-T conditions of metamorphism, implications for garnet-cordierite equilibria and the evolution of the deep crust. https://app.cochat.ai/papers/10.1007/bf01132005
- The paper
- Ellis, D. J. (1980). Osumilite-sapphirine-quartz granulites from Enderby Land, Antarctica: P-T conditions of metamorphism, implications for garnet-cordierite equilibria and the evolution of the deep crust. Contributions to Mineralogy and Petrology. https://doi.org/10.1007/bf01132005
Data sources
Bibliographic data: Semantic Scholar, OpenAlex, Crossref.
Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.
