Deutsch: Ivrea-Ceneri-Komplex
Français: Complexe Ivrea-Ceneri
Italiano: Complesso Ivrea-Ceneri
English: Ivrea-Ceneri Complex
The Ivrea-Ceneri Complex is a thick-skinned tectonic unit developped during the Alpine orogeny. It includes the lower crustal rocks of the Ivrea Zone and the WNW part of the middle to upper crustal Strona-Ceneri Zone. In the northwest, the Ivrea-Ceneri Complex is separated from the Canavese Zone by the Internal Canavese Fault, east of Locarno from the Central Alps by the Tonale Fault. In the east and southeast, the transition to the Upper Orobic Nappe is not clearly defined. The boundary can be traced along the Tamaro Thrust and the Lago Maggiore Fault. In the south, west of Lago Maggiore, the Ivrea-Ceneri Complex with its Mesozoic cover is overlain by the post-orogenic deposits of the Po Plain.
Ivrea-Ceneri Complex (TK500 / Gouffon et al. 2024)
