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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)
Tinterri, R., Muzzi Magalhaes, P., Tagliaferri, A., Cunha, R.S.Language:
english
Journal:
Sedimentary Geology
DOI:
10.1016/j.sedgeo.2016.01.023
Date:
February, 2016
File:
PDF, 7.47 MB
english, 2016