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Cycladic Massif
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The Cycladic Massif is a Miocene high-pressure orogenic segment located in the Aegean Sea underlying the Cyclades.[1] Initially, the Massif was a single island which began to break apart due to the tectonic activities of the subduction of the African Plate under the Eurasian Plate during the late Miocene Epoch.
Location
![[icon]](#/media/File:Wiki_letter_w_cropped.svg){kind=small} | This section is empty. You can help by adding to it. (December 2012) |
Geology
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Volcanos
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References
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