Climatically driven late Pleistocene – Holocene hydrological system transformation and landscape evolution in the eastern periphery of Chuya basin, SE Altai, Russia

Author:

Nepop R.K.,Agatova A.R.,Uspenskaya O.N.

Funder

Russian Foundation for Basic Research

EX-AQUA

INQUA TERPRO

Publisher

Elsevier BV

Subject

Earth-Surface Processes

Reference57 articles.

1. Geomorphologic mapping of the Chagan-Uzun River basin: a key for reconstructing history of Pleistocene glaciations in the southeastern Altai;Agatova;Stratigr. Geol. Correl.,2005

2. Pleistocene glaciations of the SE Altai, Russia, based on geomorphological data and absolute dating of glacial deposits in Chagan reference section;Agatova;Geochronometria,2017

3. Holocene glacier fluctuations and climate changes in the southeastern part of the Russian Altai (South Siberia) based on a radiocarbon chronology;Agatova;Quat. Sci. Rev.,2012

4. Outburst floods of the ice-dammed lakes in the SW of Tuva, southern Siberia;Agatova;Z. Geomorphol.,2015

5. Human occupation of South Eastern Altai highlands (Russia) in the context of environmental changes;Agatova;Archaeol. Anthropol. Sci.,2016

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