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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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
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author A. Poleshchuk
D. Zykov
S. Shvarev
author_facet A. Poleshchuk
D. Zykov
S. Shvarev
author_sort A. Poleshchuk
collection DOAJ
description 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 silt in the esker. The sand and silt were deformed with formation of recumbent and overturned folds, which indicate that they have experienced displacement in a ductile (wet) state. The formation of similar dislocations (diapir folds or glacial intrusion structures) can occur as a result of either dead ice melting or liquefaction during earthquakes.
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spelling doaj.art-0be0d866ee034a16a83a99ee219da5512022-12-22T03:11:41ZengGeological Society of FinlandBulletin of the Geological Society of Finland0367-52111799-46322018-12-0190229130010.17741/bgsf/90.2.011Some features of deformation structures in an esker on the southern margin of the Fennoscandian shieldA. PoleshchukD. ZykovS. ShvarevAs 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 silt in the esker. The sand and silt were deformed with formation of recumbent and overturned folds, which indicate that they have experienced displacement in a ductile (wet) state. The formation of similar dislocations (diapir folds or glacial intrusion structures) can occur as a result of either dead ice melting or liquefaction during earthquakes.http://www.geologinenseura.fi/bulletin/Volume90/Bulletin_vol90_2_291-300_2018_Poleshchuk-etal.pdfeskersFennoscandian Shieldliquefactionneotectonicspalaeoearthquakesdeformation structuresdislocationsintrusion
spellingShingle A. Poleshchuk
D. Zykov
S. Shvarev
Some features of deformation structures in an esker on the southern margin of the Fennoscandian shield
Bulletin of the Geological Society of Finland
eskers
Fennoscandian Shield
liquefaction
neotectonics
palaeoearthquakes
deformation structures
dislocations
intrusion
title Some features of deformation structures in an esker on the southern margin of the Fennoscandian shield
title_full Some features of deformation structures in an esker on the southern margin of the Fennoscandian shield
title_fullStr Some features of deformation structures in an esker on the southern margin of the Fennoscandian shield
title_full_unstemmed Some features of deformation structures in an esker on the southern margin of the Fennoscandian shield
title_short Some features of deformation structures in an esker on the southern margin of the Fennoscandian shield
title_sort some features of deformation structures in an esker on the southern margin of the fennoscandian shield
topic eskers
Fennoscandian Shield
liquefaction
neotectonics
palaeoearthquakes
deformation structures
dislocations
intrusion
url http://www.geologinenseura.fi/bulletin/Volume90/Bulletin_vol90_2_291-300_2018_Poleshchuk-etal.pdf
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