TETTONICA QUATERNARIA NELLA DORSALE APPENNINICA UMBRO-MARCHIGIANA E BACINI INTRAPPENNINICI ASSOCIATI

Please use this identifier to cite or link to this item: http://dx.doi.org/10.15165/studgeocam-1186

Title:	TETTONICA QUATERNARIA NELLA DORSALE APPENNINICA UMBRO-MARCHIGIANA E BACINI INTRAPPENNINICI ASSOCIATI
Authors:	CALAMITA, F. PIZZI, A.
Keywords:	Appennino umbro-marchigiano - Geologia strutturale - Tettonica quaternaria e bacini intrappenninici Umbro-Marchean Apennines, Structural Geology - Quaternary tectonics - Continental Quaternary basins development
Issue Date:	1992
Publisher:	Università di Camerino
Citation:	Studi geologici camerti, n. speciale, 1992, pp.17-25
Abstract:	The pattern of active and/ or recent normal faults and their relationship with respect to the Neogene thrusts have been analyzed in the Umbro-Marchean Apennine Ridge. Quaternary faults show en-echelon arrays and are arranged in fault zones, trending NNW-SSE (oblique with respect to the N-S oriented thrust planes), spaced 10-15 Km one from each other and ranging in length up to 30-40 Km.
URI:	http://193.204.8.201:8080/jspui/handle/1336/541
ISSN:	0392-0631
Appears in Volumess:	1992/1: "Evoluzione geomorfologica e tettonica quaternaria dell'Appennino centro-meridionale"

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STUDI GEOLOGICI CAMERTI