Some features of deformation structures in an esker on the southern margin of the Fennoscandian shield

As a result of melting of the last ice sheet in the southeastern edge of the Fennoscandian shield, ridge structures called eskers were formed. One of these eskers is the subject of our study. We have identified both typical non-deformed sedimentary layers and specific intrusive mixture of sand and s...

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Bibliographic Details
Main Authors: A. Poleshchuk, D. Zykov, S. Shvarev
Format: Article
Language:English
Published: Geological Society of Finland 2018-12-01
Series:Bulletin of the Geological Society of Finland
Subjects:
Online Access:http://www.geologinenseura.fi/bulletin/Volume90/Bulletin_vol90_2_291-300_2018_Poleshchuk-etal.pdf