tailieunhanh - Displacements and kinematics of the february 1, 1944 gerede earthquake (North Anatolian Fault System, Turkey): Geodetic and geological constraints

The North Anatolian Fault System (NAFS) is an approximately 2–110-km-wide, 1600-km-long right-lateral intra-continental transform fault boundary between the Anatolian platelet and the Eurasian plate. The Gerede fault zone is one of the major active structures in the western section of the NAFS. | Displacements and kinematics of the february 1, 1944 gerede earthquake (North Anatolian Fault System, Turkey): Geodetic and geological constraints

TỪ KHÓA LIÊN QUAN