Tectonic control of graphite mineralization in Sri Lanka

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Abstract
Summary The localization of graphite veins in well-defined regions within anticlinal structures of the SW sector of the island, where the rocks have been migmatitized partially by a reactivation, is very significant. The graphite mineralization seems to have taken place during the above mentioned reactivation and has followed regions of structural weakness developed during the folding of the metasedimentary rocks.

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