Geomorphologic and geocryologic features of the East-Siberian sector of the Arctic shelf and its development in the Late Pleistocene - Holocene
Abstract
Analysis of the geology-geomorphologic data allowed us to create a model of coasal-shelf cryolithosphere evolution in the Eastern Arctic Shelf of Eurasia (the Eastern Siberian Sea as an example) during the last 80000 years. This epoch includes two large cryochrons corresponding to the Zyryan and Satan regressions, and two thermochrons corresponding to the Karga and Holocene transgressions.
About the Authors
I. D. DanilovRussian Federation
A. Ju. Vlasenko
Russian Federation
V. Yu. Biryukov
Russian Federation
Review
For citations:
Danilov I.D., Vlasenko A.J., Biryukov V.Yu. Geomorphologic and geocryologic features of the East-Siberian sector of the Arctic shelf and its development in the Late Pleistocene - Holocene. Geomorfologiya. 2001;(1):45-53.