Abstract:<p>The Attic-Cycladic Massif (ACM) preserves the entire evolution of a NE dipping subduction zone.&#160; This includes the intra-oceanic subduction initiation associated with ophiolite obduction and formation of a metamorphic sole, to subduction-termination associated with burial and exhumation of the Cycladic continental margin to eclogite-blueschist facies conditions. The Tsiknias Ophiolite represents a piece of ca. 162 Ma Tethyan oceanic lower crust and mantle that was thrust towards t… Show more
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