Abstract
Hydrothermal graphite has been found over an area of 3,000 Km2 in New Hampshire, USA. Its pervasive presence records fluid flow of regional extent during metamorphism. Graphite precipitated from metamorphic fluids crosscuts and replaces Silurian and Devonian metasedimentary and metaplutonic rocks. The metamorphic grade of host rocks ranges from kyanite + staurolite, to sillimanite, sillimanite + alkali feldspar, or cordierite + sillimanite + alkali feldspar.
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References
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© 1989 Kluwer Academic Publishers
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Rumble, D., Chamberlain, C.P., Zeitler, P.K., Barreiro, B. (1989). Hydrothermal Graphite Veins and Acadian Granulite Facies Metamorphism, New Hampshire, USA. In: Bridgwater, D. (eds) Fluid Movements — Element Transport and the Composition of the Deep Crust. NATO ASI Series, vol 281. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-0991-5_11
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DOI: https://doi.org/10.1007/978-94-009-0991-5_11
Publisher Name: Springer, Dordrecht
Print ISBN: 978-94-010-6935-9
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