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Graphite deposits of Sri Lanka: a consequence of granulite facies metamorphism

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Abstract

The vein graphite deposits of Sri Lanka are located in a Precambrian high grade metamorphic terrain dominated by granulite facies rocks. The vein graphite has been interpreted as being of solid phase lateral secretion origin, derived by hydrothermal solutions or of biogenic origin. Based on what is known on the composition of the fluids under granulite facies conditions and the role of these fluids in their transport through the crust, the origin of the graphite is proposed to be the direct consequence of granulite facies metamorphism in the presence of a CO2 rich fluid under low fO2 conditions. This CO2 rich fluid could promote hydraulic fracturing and precipitation of vein graphite. Textures and structures of the vein graphite indicate syntectonic deposition by a crack-seal process under granulite facies metamorphic conditions. This model is supported by temperature estimates on graphite based on XRD data and stable carbon isotopes of graphite that suggest a deep-seated crustal origin.

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  1. Department of Applied Geology, University of New South Wales, P.O. Box 1, 2033, Kensington, N.S.W., Australia

    M. B. Katz

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Katz, M.B. Graphite deposits of Sri Lanka: a consequence of granulite facies metamorphism. Mineral. Deposita 22, 18–25 (1987). https://doi.org/10.1007/BF00204238

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