作者: Alice Ghiselli , Michele Zucali , Alfredo Bini
DOI: 10.1080/17445647.2014.987832
关键词: Basement (geology) 、 Scale (map) 、 Geomorphology 、 Sedimentary rock 、 Trona 、 Geology 、 Landform 、 Geological survey
摘要: We present a structural and geomorphological map of the Passo San Marco – Pizzo di Trona area (Northwestern Orobic Alps). This was studied in order to make contribution mapping interpretation landforms mesoscale structures basement sedimentary cover. The aim this study is provide useful insight for better understanding geological evolution belt during Alpine orogenesis. original survey carried out at 1:5000 scale while presented 1:8000 scale. In particular, detailed brittle ductile out. analysis has led identification six phases deformation: three pre-Alpine Alpine. During these deformation phases, (folds foliations) (faults, cataclasites pseudotachylites) developed both Variscan Permo-Triassic