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...
Kaydedildi:
| Asıl Yazarlar: | , , |
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| Materyal Türü: | Artigo |
| Dil: | Inglês |
| Baskı/Yayın Bilgisi: |
Geological Society of Finland
2018-12-01
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| Seri Bilgileri: | Bulletin of the Geological Society of Finland |
| Konular: | |
| Online Erişim: | http://www.geologinenseura.fi/bulletin/Volume90/Bulletin_vol90_2_291-300_2018_Poleshchuk-etal.pdf |
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