The erosionally confined to emergent transition in a slope‐derived blocky mass‐transport deposit interacting with a turbidite substrate, Ventimiglia Flysch Formation (Grès d’Annot System, north‐west Italy)
1979 ◽
Vol 44
◽
pp. 349-355
1968 ◽
Vol 26
◽
pp. 20-21
1990 ◽
Vol 48
(3)
◽
pp. 58-59
1996 ◽
Vol 26
(12)
◽
pp. 1364-1370
◽