Persistent rupture segmentation of the Main Marmara Fault
Sezim Ezgi Güvercin, Sylvain Barbot
原始摘要（英文原文）· Original abstract
The magnitudes and epicentral locations of earthquakes along the Main Marmara Fault, Türkiye, are governed by fault geometry, such as fault bends, and by rheological barriers like thick sedimentary sequences, according to simulations of 10,000 years of the seismic cycle.