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This document summarizes a study of normal faulting on the Greek island of Sifnos in the Aegean Sea. The study finds: 1) Early top-to-the-NE shearing between 29.4-22.8 million years ago was associated with high pressure/temperature conditions and formed a regional foliation. 2) Later, top-to-the-south shearing along the Sifnos Detachment between approximately 15-10 million years ago overprinted the earlier structures. 3) Extension was subsequently accommodated by high-angle normal faults, with the orie

Author

saeidnejad.m

Language

EN