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Left-lateral shear inside the North Gulf of Evia Rift, Central Greece, evidenced by relocated earthquake sequences and moment tensor inversion
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文摘

First time that left-lateral shear is clearly documented inside the Gulf of Evia rift.

Aftershock depths indicate a seismogenic (brittle) zone of about 15 km in depth for the Gulf of Evia rift.

The left-lateral kinematics indicates crustal strain partitioning because of E-W horizontal compression.

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