Segnalazione di sedimenti quaternari deformati in Val Pellice (TO)

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Published: Nov 6, 1989
DOI: https://doi.org/10.26382/
Keywords:
Pleistocene, seismically induced structures, Pellice Valley

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G. Collo
University of Turin, Earth Sciences Department

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".

Article Details

How to Cite
Collo, G. , trans. 1989. “Segnalazione Di Sedimenti Quaternari Deformati in Val Pellice (TO)”. Alpine and Mediterranean Quaternary 3 (1): 5-14. https://doi.org/10.26382/.
Issue
Vol. 3 No. 1 (1990): IL QUATERNARIO
Section
Articles
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How to Cite

Collo, G. , trans. 1989. “Segnalazione Di Sedimenti Quaternari Deformati in Val Pellice (TO)”. Alpine and Mediterranean Quaternary 3 (1): 5-14. https://doi.org/10.26382/.