Ancient basin plain turbidite systems may be characterized by a complex sedimentary fill made up of an alternation of compositionally different types of beds which reflect multiple sources with complex relationships to the basin. Spectacular examples of mixed siliciclastic/carbonate turbidite systems are represented by the Upper Cretaceous Helminthoid Flysch in the northern Apennines.
Extrabasinal and intrabasinal sources in siliciclastic-carbonate turbidite systems of the northern Apennines / Fontana, Daniela. - In: MEMORIE DESCRITTIVE DELLA CARTA GEOLOGICA D'ITALIA. - ISSN 0536-0242. - STAMPA. - 61:(2003), pp. 41-48.
Extrabasinal and intrabasinal sources in siliciclastic-carbonate turbidite systems of the northern Apennines.
FONTANA, Daniela
2003
Abstract
Ancient basin plain turbidite systems may be characterized by a complex sedimentary fill made up of an alternation of compositionally different types of beds which reflect multiple sources with complex relationships to the basin. Spectacular examples of mixed siliciclastic/carbonate turbidite systems are represented by the Upper Cretaceous Helminthoid Flysch in the northern Apennines.
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