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The North Anatolian Fault (NAF; Turkish: Kuzey Anadolu Fay Hattı) is an active right-lateral strike-slip fault in northern Anatolia, and is the transform boundary between the Eurasian plate and the Anatolian sub-plate. The fault extends westward from a junction with the East Anatolian Fault at the Karliova triple junction in eastern Turkey ...
Local date: 17 August 1668: Local time: Late morning: Magnitude: 7.8–8.0 M s: Epicentre: 1]: Fault: North Anatolian Fault: Type: Strike-slip: Areas affected: North Anatolia, Ottoman Empire: Max. intensity: MMI IX (Violent) [1]: Foreshocks: Yes : Aftershocks: Continued for 6 months : Casualties: 8,000 dead: Northern Anatolia was struck by a large earthquake on 17 August 1668 in the late ...
The earthquake occurred on the North Anatolian Fault, which is a fault line around 1500 km long, right-lateral, strike-slip plate boundary fault between the Eurasian plate and the Anatolian Plate that travels across the northern section of Turkey. Large earthquakes measuring 7+ magnitudes on the North Anatolian fault in the 1900s have ruptured ...
The Sea of Marmara represents a pull-apart basin in a zone of complex strike-slip tectonic interactions associated with the North Anatolian Fault. The North Anatolian Fault is a predominantly right-lateral strike-slip fault that extends from Karliova to the Gulf of İzmit. West of the gulf, the fault splits into three branches; the northernmost ...
The North Anatolian Fault Zone (NAFZ), where the earthquake occurred, is a 1,200 km (750 mi) right-lateral strike-slip fault zone. It extends from the Gulf of Saros to Karlıova. It formed around 13–11 million years ago in the eastern part of Anatolia and developed westwards.
The Sürgü-Çardak Fault is an east–west striking 160 km (99 mi) long fault that runs north of the EAF. It branches away from the EAF west of Çelikhan and extends westwards to Göksun. [ 21 ] Comprising two segments; the Sürgü Fault runs 70 km (43 mi) between Çelikhan and Nurhak; the Çardak Fault runs 90 km (56 mi) between Nurhak and ...
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Much of the country lies on the Anatolian sub-plate, a small plate bounded by two major strike-slip fault zones, the North Anatolian Fault and East Anatolian Fault. The western part of the country is also affected by the zone of extensional tectonics in the Aegean Sea caused by the southward migration of the Hellenic arc.