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Numerous (meta-)gabbroic dikes or stocks occur within the latest Neoproterozoic–early Cambrian series of the Menderes Massif (Anatolide–Tauride Block, western Turkey). These well-preserved rocks were locally converted into eclogitic metagabbros and garnet amphibolites along the contacts or shear zones. Both bulk-rock composition and compositions of igneous clinopyroxenes suggest continental tholeiitic...
High-grade gneisses from the Pulur complex in NE Turkey bear evidence for biotite-dehydration melting at 820C and 0.70.8GPa, melt segregation and near-isothermal decompression to 0.40.5GPa. During further exhumation, the rocks underwent secondary pervasive rehydration at temperatures between 400 and 230C and fluid pressures between 0.3 and 0.1GPa. Metamorphic peak conditions are dated at 331327Ma,...
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