| Autor: |
Marzec, Paweł, Golonka, Jan, Pietsch, Kaja, Kasperska, Monika, Dec, Jerzy, Cichostępski, Kamil, Lasocki, Stanisław |
| Předmět: |
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| Zdroj: |
Journal of the Geological Society; Mar2021, Vol. 178 Issue 2, p1-2, 2p |
| Abstrakt: |
The stratigraphic inventory of the Zlatne Nappe includes the Jurassic-Lower Cretaceous basinal deposits, as well as Upper Cretaceous-Neogene flysch successions deposited in the accretionary prism. Another set of regional geology remarks concerns the unification of pre-Albian deposits and names of local units by [19] We do not agree with [18] that distinguishing various formations and successions is necessary to describe the seismic image of olistoliths in the PKB. The accretionary prism formed as a result of subduction of the PKB basins under the Central Carpathian Plate ([9]) during Late Cretaceous times. The matrix is represented by Upper Cretaceous-Neogene flysch successions belonging to various tectonic units. [Extracted from the article] |
| Databáze: |
Complementary Index |
| Externí odkaz: |
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