Structural and geochemical evolution of an extensional metamorphic core complex, Paros, Greece
Lower Miocene crustal extension on the island of Paros resulted in the generation of two low-lying, north-vergent extensional detachment faults that exhumed deep levels of the ductile, partially molten crust in the footwall, whilst simultaneously accumulating lower Miocene age (Aquitanian-Burdigalia...
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University of Leicester
1999
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| Online Access: | https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.737630 |