Author Archives: tewksch

Fall field work on Syros – lots of sunshine, cats, and cool rocks!

In case you didn’t know… Syros represents a fossil subduction shear zone. Rocks were brought to eclogite facies conditions in the Eocene and exhumed through the Miocene, partially along the plate interface and partially by crustal scale low-angle normal faults of the North and West Cycladic Detachment Systems. We go there to study the structural and rheological evolution of several different

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