Here we combine the stress imparted by both the magnitude-7.8 and magnitude-7.5 earthquakes to idealized faults oriented parallel to the magnitude-7.8 source, and, therefore, similar to the broad character of the East Anatolian Fault Zone.

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Here we combine the stress imparted by both the magnitude-7.8 and magnitude-7.5 earthquakes to idealized faults oriented parallel to the magnitude-7.8 source, and, therefore, similar to the broad character of the East Anatolian Fault Zone.

Here we combine the stress imparted by both the magnitude-7.8 and magnitude-7.5 earthquakes to idealized faults oriented parallel to the magnitude-7.8 source, and, therefore, similar to the broad character of the East Anatolian Fault Zone.

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