Our findings on the 2013 Khaki earthquake in Iran suggest lithology plays a
significant role in the depth extent of slip found in reverse faults in folded belts, providing an important
control on the potential size of earthquakes.
Our findings on the 2013 Khaki earthquake in Iran suggest lithology plays a
significant role in the depth extent of slip found in reverse faults in folded belts, providing an important
control on the potential size of earthquakes.