Features of the Shear Zone Found at the Base of a Mudslide in Clay Shales.
L Comegna, L Picarelli, L Olivares, G Urciuoli
Dans les comptes rendus d’articles de la conférence: GeoQuébec 2004: 57th Canadian Geotechnical ConferenceSession: Glissements de terrain 2: | Landslides 2:
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Comegna, L, Picarelli, L, Olivares, L, Urciuoli, G (2004) Features of the Shear Zone Found at the Base of a Mudslide in Clay Shales. in GEO2004. Ottawa, Ontario: Canadian Geotechnical Society.
@inproceedings{Comegna_GEO2004_463,
author = {{Comegna, L}, {Picarelli, L}, {Olivares, L}, {Urciuoli, G}}
title = {Features of the Shear Zone Found at the Base of a Mudslide in Clay Shales.}
booktitle = {Proceedings of the 57th Canadian Geotechnical Conference}
year = {2004}
organization = {The Canadian Geotechnical Society},
address = {Ottawa, Canada} }
title = {Features of the Shear Zone Found at the Base of a Mudslide in Clay Shales.}
booktitle = {Proceedings of the 57th Canadian Geotechnical Conference}
year = {2004}
organization = {The Canadian Geotechnical Society},
address = {Ottawa, Canada} }