Segnalazione di sedimenti quaternari deformati in Val Pellice (TO)
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Abstract
This work describes the deformation structures with complex and irregular forms, observed in the silt and fine sand of Early Pleistocene outcropping in the lower Pellice Valley (TO). The structures have been interpreted as "seismically induced structures".
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How to Cite
Segnalazione di sedimenti quaternari deformati in Val Pellice (TO) (G. Collo , Trans.). (1989). Alpine and Mediterranean Quaternary, 3(1), 5-14. https://doi.org/10.26382/