Seismotectonics of the Antalya Basin and surrounding regions in eastern Mediterranean from 8 to 28 December 2013 Mw 5.0-5.8 earthquake sequence
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文摘

CMTs for 16 events are computed by applying a waveform inversion method.

The geometry of focal mechanisms reveals a thrust stress regime.

It is performed to obtain a more precise picture of the Antalya Basin stress field.

The Coulomb stress change is computed to identify the expanded stress distribution.

High-resolution hypocenter relocation of the Antalya seismic sequence is examined.

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