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-filled foredeep basin (Julian Basin or Slovenian Basin of the Slovene geologists). The Grivo...
-
2012 (v1)PublicationUploaded on: October 15, 2024
-
2010 (v1)Publication
No description
Uploaded on: October 15, 2024 -
2010 (v1)Publication
No description
Uploaded on: October 15, 2024 -
2014 (v1)Publication
The Paleogene carbonate "megabreccia" units of the Friuli Basin are composite deposits produced by catastrophic shallow-water carbonate platform collapses re-deposited in relatively deep-water inner foredeep settings developed at the front of the advancing Dinaric thrust system. These thick, basin-wide mass transport deposits (MTDs) record the...
Uploaded on: October 15, 2024