Metamorphism of the Troodos Massif, Cyprus
A wide variety of "geological evidence supports the contention that the Troodos massif, Cyprus is a fragment of Mesozoic sea-floor created at a constructive plate margin. Here, the metamorphism and geochemistry of the dyke/pillow lava sequence at the top of the igreous succession are shown to b...
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Open University
1975
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| Online Access: | https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.473036 |