The geological-structural survey of the area from Passo Valle to Forcella Venegiotta was carried out. Particular attention was paid to the detection of faults, the interactions between tectonics and Ladinian magmatism in the area and the distinction between the Moena and Contrin Formations. The deformations of possible Alpine compressive tectonics and the Deep-seated Gravitational slope deformations were also studied. The detection finally led to the evaluation of a possible reactivation of the faults with Alpine tectonics, to the discovery of diatremes at the points of intersection between the veins, as well as intrusive bodies and finally to entire slopes involved in DSGSD.
È stato svolto il rilevamento geologico-strutturale della zona da Passo Valle a forcella Venegiotta. È stata fatta particolare attenzione al rilevamento delle faglie, delle interazioni fra tettonica e magmatismo Ladinico nell'area e la distinzione tra la Formazione di Moena e quella di Contrin. Sono state anche studiate le deformazioni di possibile tettonica compressiva alpina e le deformazioni gravitative profonde di versante. Il rilevamento ha portato infine a valutare una possibile riattivazione delle faglie con la tettonica alpina, alla scoperta di diatremi nei punti di intersezione tra i filoni, oltre a dei corpi intrusivi e per finire a interi versanti coinvolti da DGPV.
Rilevamento Geologico da Passo Valles a forcella Venegiotta
GUIDOLIN, DAVIDE
2024/2025
Abstract
The geological-structural survey of the area from Passo Valle to Forcella Venegiotta was carried out. Particular attention was paid to the detection of faults, the interactions between tectonics and Ladinian magmatism in the area and the distinction between the Moena and Contrin Formations. The deformations of possible Alpine compressive tectonics and the Deep-seated Gravitational slope deformations were also studied. The detection finally led to the evaluation of a possible reactivation of the faults with Alpine tectonics, to the discovery of diatremes at the points of intersection between the veins, as well as intrusive bodies and finally to entire slopes involved in DSGSD.| File | Dimensione | Formato | |
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https://hdl.handle.net/20.500.12608/92684