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Recent temporal change in the stress state and modern stress field along the North Anatolian Fault zone (Turkey)
(Oxford University Press, 1997)
The North Anatolian Fault (NAF) is a dextral strike-slip fault which runs about 1400 km from east to west, from the Karliova triple junction to the Aegean domain. It was active during the Plio-Quaternary as a consequence ...