Cited by 34Geological and Geochemical AnalysisGeochemistry and Elemental AnalysisGroundwater and Isotope Geochemistry

Stable isotope evidence for regional-scale fluid migration in a Barrovian metamorphic terrane, Vermont, USA

Stern, Libby A., Chamberlain, C. Page, Barnett, Daniel E., Ferry, John M.·1992·Contributions to Mineralogy and Petrology

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Crossref · 10.1007/bf00310779

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  • Graphite in the neighboring Waits River Formation ranges in δ13Cgraphite from -11.9‰ to -14.3‰ and resembles the carbon isotope composition of dolomite at Ludlow.

    “Although d 13 C compositions of the graphitic schist surrounding the talc-magnesite-dolomite deposit are not available, graphite in the neighboring Waits River Formation, eastern Vermont, ranges in d 13 Cgraphite composition from 11.9 ‰ to 14.3 ‰ (Stern et al., 1992) and resemble the carbon isotope composition of dolomite at Ludlow.”

    From Clumped-isotope thermometry of magnesium carbonates in ultramafic rocks (2016) · cites this paper as Stern et al., 1992

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Authors
Stern, L. A., Chamberlain, C. P., Barnett, D. E., & Ferry, J. M.
Affiliations
  • Dartmouth College (US)
  • University of Utah (US)
  • Johns Hopkins University (US)
Venue
Contributions to Mineralogy and Petrology
Published
1992-12
Volume
112
Issue
4
Pages
475-489
ISSN
  • 0010-7999 (ISSN-L)
  • 1432-0967
OpenAlex
W1973536747
Cited by
34
References
0
Citations by year
2024: 1 · 2021: 1 · 2020: 1 · 2018: 1 · 2016: 2 · 2014: 1
FWCI
3.30
Type
journal article
Language
en
Open access
closed
Locations
Contributions to Mineralogy and Petrology (publishedVersion)
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 › Earth and Planetary Sciences › Geochemistry and Petrology › Groundwater and Isotope Geochemistry
Keywords
fluid migration, hydrothermal systems, Barrovian metamorphism, carbonate isotopes, antiform

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