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Tectonometamorphic evolution of high-pressure rocks from the island of Amorgos (Central Aegean, Greece)
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Abstract:
Structural and metamorphic data from the island of Amorgos (central Aegean Sea) show evidence for the existence of two distinct high-pressure units, the Metabasite Unit and the Basal Conglomerate Unit. These are exposed at the base of a thick marble sequence and overlying flysch deposits. The Metabasite Unit is characterized by a mineral assemblage of blue amphibole, garnet and clinopyroxene, indicating P-T conditions of 500-600 °C and >13 kbar. It is juxtaposed below car...
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CCNMatthews Newswire
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