Инд. авторы:	Dobretsov N.L., Buslov M.M., Vasilevsky A.N., Vetrov E.V., Nevedrova N.N.
Заглавие:	Cenozoic history of topography in southeastern Gorny Altai: thermochronology and resistivity and gravity records
Библ. ссылка:	Dobretsov N.L., Buslov M.M., Vasilevsky A.N., Vetrov E.V., Nevedrova N.N. Cenozoic history of topography in southeastern Gorny Altai: thermochronology and resistivity and gravity records // Russian Geology and Geophysics. - 2016. - Vol.57. - Iss. 11. - P.1525-1534. - ISSN 1068-7971. - EISSN 1878-030X.
Внешние системы:	DOI: 10.1016/j.rgg.2016.10.001; SCOPUS: 2-s2.0-84995767723; WoS: 000388102000001;
Реферат:	eng: The Central Asian Orogen was reactivated in the Cenozoic, which gave rise to mountain systems and sedimentary basins, strike-slip and thrust faults, ramps, and rift basins under the far-field effect of the India-Eurasia collision. Pre-Cenozoic structures, as well as the superposed Cenozoic deformation, are traceable in the gravity pattern. Analysis and correlation of stratigraphic, tectonic, geomorphological, and geophysical (resistivity and gravity) data from Gorny Altai and tectonic modeling on the basis of apatite fission-track thermochronology show that vertical motions have been the most active for the past 5 Ma. The uplift and subsidence produced, respectively, the Chulyshman and Ukok Plateaus with high mountains around and the the Kurai-Chuya basin between them. Gravity data suggest the existence of Late Carboniferous, Jurassic, and Cretaceous rocks found in tectonic wedges around the basin at the base of its sedimentary fill. © 2016
Ключевые слова:	strike-slip fault; resistivity and gravity fields; rampfission-track thermochronology; thrust; neotectonics; Gorny Altai; plateau;
Издано:	2016
Физ. характеристика:	с.1525-1534