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...
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 |
Similar Items
-
The Fennoscandian Shield within Fennoscandia
by: J. Donner
Published: (1996-06-01) -
Late Glacial and postglacial seismicity in the Northeastern Fennoscandian Shield: tectonic position and age of paleo-earthquakes near Murmansk
by: Svetlana B. Nikolaeva, et al.
Published: (2021-06-01) -
HETEROGENEOUS LITHOSPHERIC STRUCTURE OF THE FENNOSCANDIAN SHIELD: SEISMIC DATA
by: N. V. Sharov, et al.
Published: (2022-03-01) -
FAULT SYSTEMS IN THE UPPER CRUST OF THE FENNOSCANDIAN SHIELD, THE EAST EUROPEAN PLATFORM
by: V. S. Burtman, et al.
Published: (2020-12-01) -
Structure and genesis of the Brzuchowo Lake - Kamien Krajenski Esker
by: Adam Krupa
Published: (2016-12-01)