Please use this identifier to cite or link to this item: http://dx.doi.org/10.15165/studgeocam-1122
Title: THE NEOALPINE PHASE IN THE CARNIC ALPS: SECONDARY E-W COMPRESSIONS
Authors: VENTURINI, C.
FONTANA, C.
Keywords: Eastern Southern Alps - Carnic Alps - tectonics - neoalpine phase - palaeotectonics - Bellerophon Fm.
Sudalpino orientale - Alpi Carniche - tettonica - fase neoalpina - paleotettonica - Fm. a Bellerophon
Issue Date: 1992
Publisher: Università di Camerino
Citation: Studi geologici camerti, n. speciale, 1992, pp.271-274
Abstract: This work is about the origin of a newly discovered fold and thrust system, related to the Neoalpine phase of the Carnic Alps. The axial planes of folds trend N 170°-180°E and always dip low-angle. Interferences are clear with the well-known E-W trending folds, related to the N-S stage of the same compressio­nal phase: however, from place to place, both systems re-fold each other. Here a mechanical solution is proposed, in order to connect and explain such seerningly incompatible data.
URI: http://193.204.8.201:8080/jspui/handle/1336/477
ISSN: 0392-0631
Appears in Volumess:1992/2: "Studi preliminari all'acquisizione dati del profilo CROP 1-1A La Spezia-Alpi orientali"

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