Stable isotope evidence for regional-scale fluid migration in a Barrovian metamorphic terrane, Vermont, USA
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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
Cites
Compilation of stable isotope fractionation factors of geochemical interest
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Stranded on a Late Cambrian shoreline: Medusae from central Wisconsin
(2002) · doi:10.1130/0091-7613(2002)030 · Cited by 236 · see citing works
Self-citationA historical review of metamorphic fluid flow
Ferry, J. (1994) · doi:10.1029/94jb01147 · Cited by 119
Self-citationDipple, G., & Ferry, J. (1992) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(92)90397-2 · Cited by 112 · see citing works
Self-citationEldursi, K., Branquet, Y., Guillou-Frottier, L., & Marcoux, É. (2009) · doi:10.1016/j.epsl.2009.09.009 · Cited by 79
“During regional metamorphism, a pluton gives rise to intense second-order fluid-flow perturbation within the slower regional fluid flow (Stern et al, 1992); for active regional metamorphism, a Darcy velocity of 10-11 m.s-1 is considered to be an average value (Ingebritsen and Manning, 1999).”
BackgroundActive hydrothermal systems during the recent uplift of Nanga Parbat, Pakistan Himalaya
Chamberlain, C., Zeitler, P., Barnett, D. E., Winslow, D., Poulson, S., Leahy, T., & Hammer, J. (1995) · Journal of Geophysical Research Atmospheres · doi:10.1029/94jb02062 · Cited by 58 · see citing works
Self-citationOxygen isotope constraints on metamorphic fluid flow, Townshend Dam, Vermont, U.S.A.
Kohn, M., & Valley, J. (1994) · doi:10.1016/0016-7037(94)90249-6 · Cited by 53
Clumped-isotope thermometry of magnesium carbonates in ultramafic rocks
García del Real, P., Maher, K., Kluge, T., Bird, D. K., Brown, G. E., & John, C. M. (2016) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2016.08.003 · Cited by 50 · see citing works
Cartwright, I., Vry, J., & Sandiford, M. (1995) · Contributions to Mineralogy and Petrology · doi:10.1007/bf00306509 · Cited by 39 · see citing works
Metamorphic P‐T paths from calcic pelitic schists from the Strafford Dome, Vermont, USA
Ménard, T., & Spear, F. (1994) · doi:10.1111/j.1525-1314.1994.tb00061.x · Cited by 33
Eldursi, K., Chi, G., Bethune, K., Li, Z.-H., Ledru, P., & Quirt, D. (2020) · Mineralium Deposita · doi:10.1007/s00126-020-00979-5 · Cited by 31
Wickham, S., & Peters, M. (1992) · Contributions to Mineralogy and Petrology · doi:10.1007/bf00310955 · Cited by 29 · see citing works
Ferry, J. M., Kitajima, K., Strickland, A., & Valley, J. W. (2014) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2014.08.021 · Cited by 26 · see citing works
Self-citationLéger, A., Mathez, E. A., Duba, A. G., Pineau, F., & Ginsberg, S. (1996) · Journal of Geophysical Research Atmospheres · doi:10.1029/96jb01757 · Cited by 31 · see citing works
Evans, K., Bickle, M., Skelton, A., Hall, M., & Chapman, H. (2002) · doi:10.1046/j.1525-1314.2002.00403.x · Cited by 24
“CM with relatively heavy d13C was also observed by Stern et al. (1992) and Leger et al. (1996).”
BackgroundInfluentialBuick, I., & Cartwright, I. (1996) · Journal of Petrology · doi:10.1093/petrology/37.5.1097 · Cited by 24 · see citing works
Cartwright, I., & Buick, I. (1996) · doi:10.1111/j.1525-1314.1996.00289.x · Cited by 23
Buick, I., Cartwright, I., & Williams, I. (1997) · Journal of Petrology · doi:10.1093/petroj/38.7.877 · Cited by 22 · see citing works
Polyphase metamorphic fluid flow in the Lower Calcsilicate Unit, Reynolds Range, central Australia
Cartwright, I., Buick, I., & Vry, J. (1996) · Precambrian Research · doi:10.1016/0301-9268(95)00055-0 · Cited by 20 · see citing works
Cui, W.-L., Guo, J., Huang, G.-Y., Wang, Z.-C., Liu, Y.-H., & Yang, J.-H. (2021) · Ore Geology Reviews · doi:10.1016/j.oregeorev.2021.104624 · Cited by 18
Ferry, J. (2007) · doi:10.2138/am.2007.2429 · Cited by 15
“…the area of Figure 1 and nearby have been the subject of numerous studies of ß uid-rock interaction during regional metamorphism (Ferry 1988, 1992, 1994; Chamberlain et al. 1990; Barnett and Chamberlain 1991; Stern et al. 1992; Vyhnal and Chamberlain 1996; Evans and Bickle 1999; Evans et al. 2002).”
BackgroundSelf-citationFluid flow in metamorphic environments
Young, E. (1995) · doi:10.1029/95rg00601 · Cited by 12
The link between oxygen isotope resetting, partial melting, and fluid flow in metamorphic terrains
Cartwright, & Buick (1998) · doi:10.1046/j.1365-3121.1998.00171.x · Cited by 11
“…and the systematic lowering of d18O values by several permil with increasing metamorphic grade in Vermont (USA) and the Mount Lofty Ranges (Australia) have been interpreted as being caused by synmetamorphic up-temperature fluid flow (Ferry, 1992; Stern et al., 1992; Cartwright et al., 1995).”
BackgroundMiller, J., & Cartwright, I. (1997) · Journal of the Geological Society · doi:10.1144/gsjgs.154.5.0839 · Cited by 7
“Other processes, such as devolatilization during prograde metamorphism and partial melting, can also lower ä18O values, but generally by less than 2‰ (Chamberlain et al. 1990; Stern et al. 1992; Kohn 1993).”
BackgroundCartwright, I., Buick, I., & Vry, J. (2001) · Geological Society Special Publication · doi:10.1144/gsl.sp.2001.184.01.18 · Cited by 7
“However, in a number of terrains (e.g. Mount Lofty Ranges, Australia; New England, USA; Trois Seigneurs, FranceSpain; Lizzies Basin, USA; Naxos, Greece) the progress of mineral reactions, the systematic lowering of 5180 values with metamorphic grade, and/or the occurrence of migmatites formed by fluid-present melting…”
BackgroundInfluentialReactive dispersion of stable isotopes by mineral reaction during metamorphism
Dipple, G. M. (1998) · Geochimica et Cosmochimica Acta · doi:10.1016/s0016-7037(98)00265-8 · Cited by 5 · see citing works
Vry, J., & Cartwright, I. (1998) · doi:10.1111/j.1525-1314.1998.00169.x · Cited by 5
“Unravelling the early tectonic history requires fluids derived by metamorphic devolatilization at low grades (Stern et al., 1992; Cartwright et al., 1995); the application of a variety of techniques, including detailed textural studies, stable and radiogenic isotopes, incursion of surface-derived fluids (Wickham & Tay…”
BackgroundInfluentialThe time-integrated history of crustal fluid flow: Reynolds Range, central Australia
Cartwright, I., Buick, I., & Vry, J. (2000) · doi:10.1016/s0375-6742(00)00091-1 · Cited by 4
Slack, J. F., Shanks, W., & Woodruff, L. (2024) · Economic Geology · doi:10.5382/econgeo.5106 · Cited by 3 · see citing works
Cartwright, I., & Harper, S. (1998) · doi:10.1080/08120099808728450 · Cited by 2
- 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)
- ORCID
- Stern, Libby A.
- 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
- Licence
- www.springer.com/tdm (tdm)
- 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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