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Stable carbon isotopes in selected granitic, mafic, and ultramafic igneous rocks
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“Fig. 10b shows the calculated d 13 CCO2(g) values for California (Red Mountain), Austrian, Turkish, and Iranian cryptocrystalline magnesite, which exhibit values that broadly correspond to d 13 C compositions of organic sources (plant CO2, soil, petroleum) and carbon contained in silicate and oxide minerals that constitute representative ultramafic rocks ( i.e. non-carbonate CO2 in Fuex and Baker,”
From Clumped-isotope thermometry of magnesium carbonates in ultramafic rocks (2016) · cites this paper as Fuex and Baker, 1973
Citations
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“This is similar to δ13C –7 ‰ values considered to represent upper mantle degassing CO2 (Galimov, 1968; Fuex and Baker, 1973).”
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“Surveys of the carbon isotopic compositions of igneous rocks have been reported in Hoefs (1973) and Fuex and Baker (1973) .”
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“-2.5% to -7% according to Galimov (1968) and Fuex and Baker (1973), continental dessert environments, e.g., Permian: -6% to -1% (Pierre et al. 1984), and clearly differ from fluids derived from thermally matured organic matter of typically -40% to -10% (Irwin et al. 1977), so the generally heavy…”
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“The δC value of average crustal carbon is estimated to be about −7‰ on the basis of geochemical balance calculations (Craig, 1953; Fuex and Baker, 1973).”
BackgroundImai, A., & Uto, T. (2002) · Resource Geology · doi:10.1111/j.1751-3928.2002.tb00148.x · Cited by 24
“Morishita (1993) argued that the δ13C value of hydrothermal solution for the Kushikino deposit was lower than the δ13C value of average crustal carbon (ca. –7 ‰; Craig, 1953; Fuex and Baker, 1973) and of deep-seated source or the upper mantle (ca. –7 ‰; Taylor et al., 1967; Pineau et al., 1976).”
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“…GROUP-2 veins; (ii) cements precipitated from magmatic-derived fluids (i.e. with strong influence of mantle derived CO2) display characteristically low d13C (down to 7; e.g. Horton et al. 2012) as d13C values of magmatic CO2 typically range between 7.5 and 5.5 (Galimov 1968; Fuex & Baker 1973).”
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“All data fall within the magmatic range (−10.3‰ to 2.9‰) (Craig 1953; Ohmoto 1972; Fuex and Baker 1973; Rollinson 1993; Itoh and Hanari 2010), indicating that the hydrothermal fluids from which calcites precipitated were derived from the granitic magma.”
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“The calculated d13C value of -6.5‰ for the fluid is similar to the average value for crustal carbon (e.g. Craig, 1953; Fuex & Baker, 1973) and that for © 2010 The Authors Resource Geology © 2010 The Society of Resource Geology 369 deep-seated sources or the upper mantle (e.g. Taylor et al., 1967;…”
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“The present results show that all d13C values of calcites from the Furong tin deposit fall within the range between mantle or magmatic carbon (-3 to -9‰) (Ohmoto, 1972; Rollinson, 1993), crustal carbon (Craig, 1953; Fuex & Baker, 1973) and marine carbonate.”
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“The carbon isotopic ratio of the Kushikino hydrothermal fluid was relatively low because of the basement sedimentary rocks of the Shimanto Supergroup (Morishita, 1993), while the carbon isotopic ratio of the Sakonishi hydrothermal fluid was similar to that of the earth crustal mean (about –7‰, Craig, 1953; Fuex and Ba…”
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“, [28]) instead of to that of limestone [20].”
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“Carbon dioxide is a minor component in magmas, and carbon is typically present in igneous rocks only as trace carbonate and reduced carbon (Fuex and Baker 1973; Hoefs 1973).”
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Carbon in mineralized ultramafic intrusions, caledonides, northern Britain
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Kiyosu, Y., & Wada, H. (1978) · doi:10.2465/ganko1941.73.33
Metadata
- Authors
- Fuex, A. N., & Baker, D. R.
- Affiliations
- Shell (United States) (US)
- Rice University (US)
- Venue
- Geochimica et Cosmochimica Acta
- Publisher
- Elsevier BV
- Published
- 1973-11
- Volume
- 37
- Issue
- 11
- Pages
- 2509-2521
- ISSN
- 0016-7037 (ISSN-L)
- OpenAlex
- W2003781710
- Cited by
- 56
- References
- 0
- Citations by year
- 2023: 1 · 2022: 1 · 2021: 1 · 2020: 2 · 2017: 2 · 2016: 4 · 2015: 1 · 2014: 1 · 2013: 1
- FWCI
- 1.05
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Geochimica et Cosmochimica Acta (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Keywords
- stable carbon isotopes, carbon-13, carbonate carbon, acid decomposition, isotope fractionation, mantle carbon, mafic-ultramafic rocks, isotopic equilibration, mantle degassing
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