Graphite and carbonates in the 3.8 Ga old Isua Supracrustal Belt, southern West Greenland
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Isua magnesite and dolomite δ13C values are virtually identical (-3.2‰ and -3.3‰) and consistent with other reported Isua metacarbonates (-7.6‰ to -1.1‰).
“The d 13 Cmag and d 13 Cdol values are virtually identical, 3.2 ‰ and 3.3 ‰ , respectively, and consistent with other reported metacarbonates in Isua that range in d 13 C from 7.6 ‰ to 1.1 ‰ (Van Zuilen et al., 2003).”
From Clumped-isotope thermometry of magnesium carbonates in ultramafic rocks (2016) · cites this paper as Van Zuilen et al., 2003
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- Authors
- van Zuilen, M. A., Lepland, A., Teranes, J., Finarelli, J., Wahlen, M., & Arrhenius, G.
- Affiliations
- Geological Survey of Norway (NO)
- Scripps Institution of Oceanography (US)
- University of Chicago (US)
- Venue
- Precambrian Research
- Publisher
- Elsevier BV
- Published
- 2003-10
- Volume
- 126
- Issue
- 3-4
- Pages
- 331-348
- ISSN
- 0301-9268 (ISSN-L)
- OpenAlex
- W2034834320
- Cited by
- 154
- References
- 60
- Citations by year
- 2026: 3 · 2025: 7 · 2024: 7 · 2023: 8 · 2022: 5 · 2021: 9 · 2020: 6 · 2019: 6 · 2018: 12 · 2017: 4 · 2016: 8 · 2015: 5 · 2014: 4 · 2013: 8 · 2012: 7
- FWCI
- 6.43
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Precambrian Research (publishedVersion)
- Funders
- Comisión de Investigaciones Científicas
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Origins and Evolution of Life
- Keywords
- graphite, carbonates, Isua supracrustal belt, early Archean, metacarbonates, carbon isotope ratio, metasomatism, banded iron formations, metachert, magnetite, metamorphic temperature
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