Please use this identifier to cite or link to this item:
http://dx.doi.org/10.15165/studgeocam-805
Title: | CARATTERI GEOLOGICO-STRUTTURALI DELL'AREA PEDEAPPENNINICA MARCHIGIANO-ABRUZZESE DURANTE IL PLEISTOCENE |
Authors: | BIGI, S. CENTAMORE, E. NISIO, S. |
Keywords: | Bacino periadriatico - Pleistocene - evoluzione tettonica Periadriatic basin - Pleistocene - tectonic evolution |
Issue Date: | 1996 |
Publisher: | Università di Camerino |
Citation: | Studi geologici camerti, 14, 1996, pp.193-200 |
Abstract: | The Pleistocene tectonic evolution ofthe Marchean-Abruzzi sector of the Periadriatic basin is the result of severa! mechanisms acting at the same time, during the final fases of the structuring of the Apennine chain. These mechanisms contro! the sedimentary evolution of the basin, the distribution of the sedimentary environments and the morphostructural setting of the continental landscape. [...] |
URI: | http://193.204.8.201:8080/jspui/handle/1336/150 |
ISSN: | 0392-0631 |
Appears in Volumess: | Volume 14 (1996-97) |
Files in This Item:
File | Description | Size | Format | |
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Vol. 14 Capitolo 12.pdf | 14, 1996, pp.193-200 | 1,27 MB | Adobe PDF | View/Open |
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