Geodynamic effects detected in the Stolowe Góry Mountains investigated originally for gravitational mass movements /
Rock block forms of the Szczeliniec Wielki (919 m a.s.l.) in the border area of the Stolowe Mountains massif originated due to various exogenous and endogenous pro cesses. The processes had started in the Upper Cretaceous, culminated in Late Tertiary, and continue till the present day with much lowe...
| Hlavní autor: |
Cacoń, Stefan
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Autor )
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| Další autoři: |
Košťák, Blahoslav
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Autor )
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| Typ dokumentu: | Článek |
| Jazyk: |
angličtina |
| ISSN: | 1214-9705 |
| Zdroj: | Acta geodynamica et geomaterialia: Vol. 9, no. 4 (168)(2012), s. 457-472. |
| Předmět: | |
| Externí odkaz: |
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