Cryogenic Deformation Structures in Late Cenozoic Unconsolidated Sediments of the Tunka Depression in the Baikal Rift Zone

Author:

Alexeev Sergey1,Alexeeva Ludmila1,Kononov Alexander1

Affiliation:

1. Institute of the Earth's Crust of the Siberian Branch of the Russian Academy of Sciences (IEC SB RAS); Irkutsk Russian Federation

Publisher

Wiley

Subject

Earth-Surface Processes

Reference32 articles.

1. The evolution of permafrost in the western part of the Todzha depression, Russia;Alexeev;Geomorphology,2007

2. Convective deformations formation in poorly lithified sedimentary rocks;Artyushkov;Izvestiya AN USSR, ser. geol.,1965

3. Baikal Branch of the Geophysical Survey, Siberian Branch of the Russian Academy of Sciences 2013 http://www.seis-bykl.ru

4. Grundzüge der Quartärgeologie Mitteldeutschlands (Sachsen, Sachsen Anhalt, Südbrandengurg, Türingen);Eissman;Altenburger Naturwissenschaftliche Forshungen,1994

5. Present-day notions of the permafrost region evolution in Western and Eastern Siberia during Pleistocene and Holocene (Message 2);Fotiev;Earth Cryosphere,2006

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