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Heinsalu & Bednarczyk, 1997
Tremadoc of the East European Platform: lithofacies and palaeogeography
Heinsalu, H., Bednarczyk, W.
| DOI | 10.3176/geol.1997.2.01 |
|---|---|
| Year | 1997 |
| Title translated | Tremadoc Ida-Euroopa platformil: litofaciaalsus ja paleogeograafia |
| Journal | Proceedings of the Estonian Academy of Sciences. Geology |
| Volume | 46 |
| Number | 2 |
| Pages | 59-74 |
| Type | article in journal |
| Figures | 2 |
| OpenAccess | |
| Estonian author | |
| Language | English |
| Id | 1049 |
Abstract
In the Tremadoc the palaeobasin of the East European Platform was a NW-SE elongated inland sea between the Baltic and Ukrainian shields. It opened into the Iapetus Ocean in NNW. The present Moscow Syneclise may have had a connection with the Palaeo-Ural Sea, too. Terrigenous sedimentation represented by sandy-silty and pelitic material predominated. On the basis of the sediments preserved, we can distinguish three main regions with different sedimentary conditions in the Tremadoc basin: Scandinavia-Poland, Northern East Baltic, Moscow Syneclise.
Last change: 28.11.2022