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In the pennidic metamorphic formation M. Forno Amphibolite pillow structures have been discovered near the Passo del Muretto on the Italian-Swiss border. The cores of the pillows, completely homogeneous because of the metamorphism, are made up by an actinolitic hornblende and by plagioclase (32 % An). In the variolitic borders, consisting of actinolitic hornblende, plagioclase (28 % An) and epidote, textural and mineralogical gradations, both of primary and metamorphic origin, are evident. The interpillow...
The sedimentary wedges of the Insubric Line near Dubino and in the upper S. Jorio valley have been studied in detail. They are the only ones having a clear stratigraphic sequence, that may be correlated with the Permian and Triassic rock series of the Orobic Alps. In the Dubino wedge the lower Permian has been ascertained: it occurs as tuffaceous sandstone of the type of the Collio formation. Within the upper S. Jorio valley profile the variegated siltstone unit appear to belong to the Servino formation...
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