Conglomérats polygéniques ophiolitiques: anciens éboulis de talus de fond océanique?
1981 ◽
Vol 18
(3)
◽
pp. 619-623
◽
Keyword(s):
Field observations on the polygenetic conglomerates associated with the ophiolitic complexes in the Eastern Townships are comparable to those on the common slope facies in the present-day ocean bottom. Sedimentary processes (submarine erosion, deposition) are probably responsible for the internal structures of the conglomerates. This working hypothesis replaces the explosion-origin interpretation previously proposed. [Journal Translation]