The relationship between triassic magmatic bodies of the west side of Monte Guglielmo with tectonic elements is here studied in deep. The measurements were performed on outcrops of such magnitude that they can be considered sufficiently representative of the relations existing between the magmatic bodies, faults and surrounding formations. Thus, it is seen that the outcrops have a total orientation NNW/SSE and a dip of 30°, although some exceptions. Volcanites appear to be linked to the action of the Monte Guglielmo Line, a little known fault about which we will do more detailed studies.

Monte Guglielmo (Brescia): relazione tra le faglie e le vulcaniti triassiche del versante sud-occidentale. = Monte Guglielmo (Brescia): Relationship faults and Triassic volcanites of the south-western mountainside.

Buffoli, Gabriele
2014/2015

Abstract

The relationship between triassic magmatic bodies of the west side of Monte Guglielmo with tectonic elements is here studied in deep. The measurements were performed on outcrops of such magnitude that they can be considered sufficiently representative of the relations existing between the magmatic bodies, faults and surrounding formations. Thus, it is seen that the outcrops have a total orientation NNW/SSE and a dip of 30°, although some exceptions. Volcanites appear to be linked to the action of the Monte Guglielmo Line, a little known fault about which we will do more detailed studies.
2014-09-17
25
Guglielmo, Brescia, Vulcaniti triassiche, Sovrascorrimenti
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.12608/18736