Anatomy of the Cycladic Blueschist Unit on Sifnos Island (Cyclades, Greece)
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文摘

The CBU of Sifnos shows different degree of retrogression of HP-LT parageneses.

Shearing was characterized by localization of strain toward the base of tectonic pile.

Eocene shear zones were deformed and/or reactivated during post-orogenic exhumation with top-to-the-NE shearing.

Late low-angle and steeper normal faults may be the brittle expression of the WCDS.

The localization of strain occurred at the Eocene within the subduction channel.

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