Инд. авторы:	Deev E.V., Zolnikov I.D., Goltsova S.V., Rusanov G.G., Emanov A.A.
Заглавие:	Traces of paleoearthquakes in the Quaternary deposits of intermontane basins in central Gorny Altai
Библ. ссылка:	Deev E.V., Zolnikov I.D., Goltsova S.V., Rusanov G.G., Emanov A.A. Traces of paleoearthquakes in the Quaternary deposits of intermontane basins in central Gorny Altai // Russian Geology and Geophysics. - 2013. - Vol.54. - Iss. 3. - P.312-323. - ISSN 1068-7971. - EISSN 1878-030X.
Внешние системы:	DOI: 10.1016/j.rgg.2013.02.006; SCOPUS: 2-s2.0-84875403548; WoS: 000316855700006;
Реферат:	eng: Study of the sections of Neopleistocene-Holocene deposits filling the basins in central Gorny Altai has revealed earthquake-induced soft-sediment deformation (seismites). They formed as a result of the brittle deformation of deposits and liquefaction of loose water-saturated sediments under vibration seismic impact. The paleoearthquakes resulting in such seismites had the minimum intensity I = 6 and magnitude M = 5-6. Hence, the study region underwent strong earthquakes in the Neopleistocene-Holocene. © 2013.
Ключевые слова:	Earthquakes; Holocene; Russian Federation; Altay [Russian Federation]; seismite; seismicity; Quaternary; Pleistocene-Holocene boundary; paleoseismicity; neotectonics; intermontane basin; earthquake mechanism; earthquake magnitude; deformation mechanism; brittle deformation; Seismites; Neotectonics; Central Gorny Altai; Neopleistocene;
Издано:	2013
Физ. характеристика:	с.312-323