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Supershear transition due to a free surface in 3-D simulations of spontaneous dynamic rupture on vertical strike-slip faults
Supershear transition Earthquake rupture dynamics Earthquake source physics
2014/4/8
Supershear rupture propagation has been inferred from seismic observations for natural faults and observed in laboratory experiments. We study the effect of the free surface on the transition of earth...
The June 6, 2000, Orta (Çankırı, Turkey) Earthquake: Sourced from a New Antithetic Sinistral Strike-slip Structure of the North Anatolian Fault System, the Dodurga Fault Zone
North Anatolian Fault System Antithetic Fault Sinistral Strike-slip Fault Orta Earthquake
2009/7/8
The İsmetpaşa-Kargı section of the North Anatolian Fault System (NAFS) consists of six subfault zones, namely the Eskipazar, the Ulusu, the Tosya, the Çerkeş-Kurşunlu, ...
The Role of Crustal Fluids in Strike-slip Tectonics: New Insights from Magnetotelluric Studies
crustal fluids magnetotelluric strike-slip tectonics transform plate boundaries crustal deformation
2009/7/8
The presence of fluids in the Earth's crust can dramatically change the rheology and may control a wide range of tectonic processes, especially in regions characterized by strike-slip deformation. Flu...
Different Modes of Stress Transfer in a Strike-slip Fault Zone: an Example From the North Anatolian Fault System in Turkey
North Anatolian Fault System (NAFS) strike-slip faulting earthquake stress transfer
2009/7/7
The dextral North Anatolian Fault System (NAFS) extends for well over 1000 km from the compressive tectonic domain of eastern Anatolia into the broad and diverse tectonic domain of the western Anatol...