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Dragovic, Besim, Gatewood, Matthew P., Baxter, Ethan F., Stowell, Harold H. (2018) Fluid production rate during the regional metamorphism of a pelitic schist. Contributions to Mineralogy and Petrology, 173 (11) doi:10.1007/s00410-018-1523-9

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Reference TypeJournal (article/letter/editorial)
TitleFluid production rate during the regional metamorphism of a pelitic schist
JournalContributions to Mineralogy and Petrology
AuthorsDragovic, BesimAuthor
Gatewood, Matthew P.Author
Baxter, Ethan F.Author
Stowell, Harold H.Author
Year2018 (November)Volume173
Issue11
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s00410-018-1523-9Search in ResearchGate
Mindat Ref. ID80129Long-form Identifiermindat:1:5:80129:0
GUIDac8107bc-dc76-4e4d-88be-eec2cb543686
Full ReferenceDragovic, Besim, Gatewood, Matthew P., Baxter, Ethan F., Stowell, Harold H. (2018) Fluid production rate during the regional metamorphism of a pelitic schist. Contributions to Mineralogy and Petrology, 173 (11) doi:10.1007/s00410-018-1523-9
Plain TextDragovic, Besim, Gatewood, Matthew P., Baxter, Ethan F., Stowell, Harold H. (2018) Fluid production rate during the regional metamorphism of a pelitic schist. Contributions to Mineralogy and Petrology, 173 (11) doi:10.1007/s00410-018-1523-9
In(2018, November) Contributions to Mineralogy and Petrology Vol. 173 (11) Springer Science and Business Media LLC

References Listed

These are the references the publisher has listed as being connected to the article. Please check the article itself for the full list of references which may differ. Not all references are currently linkable within the Digital Library.

Not Yet Imported: Treatise on Geochemistry - book-chapter : 10.1016/B978-0-08-095975-7.00306-5

If you would like this item imported into the Digital Library, please contact us quoting Journal ID
Armstrong JT (1984) Quantitative Analysis of silicate and oxide minerals: a reevaluation of ZAF corrections and proposal for Bencee-Albee coefficients. In: Microbeam Analysis. San Francisco Press, California
Armstrong TR (1992) Progressive evolution of Acadian dynamothermal events in southern Vermont: evidence for the trangressive dome developmnent. Geol Soc Am Abstract Prog 24:4
Baxter EF (2003) Natural constraints on metamorphic reaction rates. In: Vance D, Muller W, Villa IM (eds) Geochronology: linking the isotopic record with petrology and textures, vol 220. Geological Soc Publishing House, Bath, pp 183–202
Doll CG, Cady WM, Thompson JB, Billings MP (1961) Centennial Geologic Map of Vermont. In. vol. Vermont Geological Survey, Montpelier
Karabinos P, Laird J (1988) Structure and metamorphism from Jamaica to the Chester Dome, Vermont. In: New England Intercollegiate Geologic Conference, Guidebook for Fieldtrips, Bothner, WA, pp 281–292
Kohn MJ, Spear FS (1990) Two new geothermometers for garnet amphibolites, with applications to southeastern Vermont. Am Miner 75(1–2):89–96
Not Yet Imported: Journal of Petrology - journal-article : 10.1093/petrology/egx039

If you would like this item imported into the Digital Library, please contact us quoting Journal ID 45855
Radcliffe N, Armstrong TR, Tracy RJ (1992) Relations between tectonic-cover and basement, and metamorphic conditions of formation of the Sadawga, Rayponda, and Athens Domes of southern Vermont. In: Robinson P, Brady JB (eds) Guidebook for Field Trips in the Connecticut Valley Region of Massachusetts and Adjacent States, 2. vol. Department of Geology and Geophysics, University of Massachusetts, Amherst, pp 257–290
Rosenfeld JL (1968) Garnet rotations due to the major Paleozoic deformations in southeast Vermont. In: Zen E (ed) Studies of Appalachain Geology: Northern and Maritime. Wiley, New York, pp 185–202
Tracy RJ, Rye DM, Hewitt DA, Schiffries CM (1983) Petrologic and stable-isotopic studies of fluid-rock interactions, south-central Connecticut: I. The role of infiltration in producing reaction assemblages in impure marbles. Am J Sci 283A:589–616
Yardley BWD (1986) Fluid Migration and Veining in the Connemara Schists, Ireland. Springe, New York, pp 109–131


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