Quaternary faulting in the Tatra Mountains, evidence from cave morphology and fault-slip analysis

Quaternary faulting in the Tatra Mountains, evidence from cave morphology and fault-slip analysis

Tectonically deformed cave passages in the Tatra Mts (Central Western Carpathians) indicate some fault activity during the Quaternary. Displacements occur in the youngest passages of the caves indicating (based on previous U-series dating of speleothems) an Eemian or younger age for those faults, an...

Πλήρης περιγραφή

Λεπτομέρειες βιβλιογραφικής εγγραφής
Κύριος συγγραφέας:	Szczygieł Jacek
Μορφή:	Άρθρο
Γλώσσα:	English
Έκδοση:	Earth Science Institute, Slovak Academy of Sciences, Slovakia 2015-06-01
Σειρά:	Geologica Carpathica
Θέματα:	neotectonics Quaternary faults stress tensor uplift cave Tatra Mts Western Carpathians
Διαθέσιμο Online:	http://www.degruyter.com/view/j/geoca.2015.66.issue-3/geoca-2015-0023/geoca-2015-0023.xml?format=INT

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