In the Northern Apennines of Italy, mud-rich olistostromes (sedimentary melanges) occur at different stratigraphic levels within the late Oligocene-early Miocene sedimentary record of episutural/wedge-top basins. They are widely distributed along the exhumed outer part of the Ligurian accretionary complex, atop the outer Apenninic prowedge,...
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2015 (v1)PublicationUploaded on: October 15, 2024
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2016 (v1)Publication
In this study we combine observations and analytical data from large-scale (10-100s of m-thick and 100 m(2)-extensive), siliciclastic and carbonate MTD/MTCs belonging to the Oligocene - Miocene foredeep and wedge-top successions of the Northern Apennines and the Paleocene - Eocene Friuli basin of the northwestern Dinarides (Italy and Slovenia),...
Uploaded on: November 2, 2024 -
2016 (v1)Publication
Olistostromes (sedimentary mélanges) represent the products of ancient submarine mass transport processes. We present a comparative analysis of the occurrences and internal structures of these sedimentary mélanges at a global scale with a focus on the Circum-Mediterranean, Appalachian and Circum-Pacific regions, and discuss their formation and...
Uploaded on: November 2, 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