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pro vyhledávání: '"Kinematics of emplacement"'
The Paleogene carbonate megabreccias of the Eastern Friuli, South-Eastern Alps of Italy, are thick, up to 260 m, and laterally extensive, up to 100 km, bodies attributed to catastrophic submarine landslides, which occurred in a deep-water, turbidite-
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::54c55d4563dea1b210767c9e2c7dfd8c
https://hdl.handle.net/11368/2695990
https://hdl.handle.net/11368/2695990
