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...
Main Author: | |
---|---|
Published: |
Open University
1975
|
Subjects: | |
Online Access: | https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.473036 |