e-Article
Convolute laminations and load structures in turbidites as indicators of flow reflections and decelerations against bounding slopes. Examples from the Marnoso-arenacea Formation (northern Italy) and Annot Sandstones (south eastern France)
Document Type
Article
Source
In Sedimentary Geology October 2016 344:382-407
Subject
Language
ISSN
0037-0738