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Structural-tectonic architecture of limestone quarry Gombasek on Plešivec Plateau of Silica Nappe
Investigation of bends, fold deformations, sigmoidal foliation trend as well as displacement of Silica Nappe surfaces revealed gradual evolution of Late Cretaceous tectonic movements in the limestone quarry Gombasek located on Plešivec Plateau of Silica Nappe. Tertiary and recent tectonic changes resulted in extension, fault polishes of semiductile deformation, reactivation of tectonic structures, formation of horst and graben structures and extensional structures of karstification.
Structural-tectonic architecture of limestone quarry Gombasek on Plešivec Plateau of Silica Nappe
Investigation of bends, fold deformations, sigmoidal foliation trend as well as displacement of Silica Nappe surfaces revealed gradual evolution of Late Cretaceous tectonic movements in the limestone quarry Gombasek located on Plešivec Plateau of Silica Nappe. Tertiary and recent tectonic changes resulted in extension, fault polishes of semiductile deformation, reactivation of tectonic structures, formation of horst and graben structures and extensional structures of karstification.
Structural-tectonic architecture of limestone quarry Gombasek on Plešivec Plateau of Silica Nappe
Julián Kondela (Autor:in) / Stanislav jun. Jacko (Autor:in) / Tibor Sasvári (Autor:in)
2006
Aufsatz (Zeitschrift)
Elektronische Ressource
Unbekannt
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