首页> 外文期刊>Geologia >JURASSIC TO LOWER CRETACEOUS DEPOSITS OF THE PIENINY KLIPPEN BELT AND MANIN UNIT IN THE MIDDLE VAH VALLEY (BIELE KARPATY AND STRAZOVSKE VRCHY MTS, WESTERN SLOVAKIA)
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JURASSIC TO LOWER CRETACEOUS DEPOSITS OF THE PIENINY KLIPPEN BELT AND MANIN UNIT IN THE MIDDLE VAH VALLEY (BIELE KARPATY AND STRAZOVSKE VRCHY MTS, WESTERN SLOVAKIA)

机译:瓦赫河谷中部的纪里布纪克利彭带和Manin单元的侏罗纪至下白垩纪沉积(斯洛伐克西部的比勒·卡帕蒂和斯特拉佐夫斯基·维奇)

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摘要

In the Western Slovakia, the Pieniny Klippen Belt (PKB) is morphostructurally divided into four sectors: Podbranc-Trencin, Puchov, Varin and Orava, which differ in their inner structure and in presence of the individual units. The geological and tectonic division of the PKB is however more complex. Numerous units, developments, lithostratigraphic and tectonic units have been distinguished during long-term investigations (e.g. Birkenmajer 1977, Misik et al. 1996).
机译:在斯洛伐克西部,Pieniny Klippen带(PKB)在形态结构上分为四个部分:Podbranc-Trencin,Puchov,Varin和Orava,它们的内部结构和单个单元均不同。但是,PKB的地质和构造划分更为复杂。在长期调查中,已经区分出许多单元,发育,岩石地层学和构造单元(例如Birkenmajer 1977,Misik等人1996)。

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