Turbidites mega-beds are the product of convulsive sedimentary events and provide time lines for the study of the stratigraphic record. An integrated and detailed study of depositional facies, petrography. paleontology and geochemistry of Cassio mega-beds allows: 1) determination of individual sediment types stored before resedimentation: 2) recognition of source area locations, types of triggering mechanisms, and transport/depositional processes, bottom fauna ecologu and diagenetic modifications.

Anatomy of carbonate turbidite mega-beds (M. Cassio Formation, Upper Cretaceous, northern Apennines, Italy) / Zuffa, G. G.; Fontana, Daniela; Morlotti, E.; PREMOLI SILVA, I.; Sighinolfi, G. P.; Stefani, C. FONTANI L.. - In: MEMORIE DESCRITTIVE DELLA CARTA GEOLOGICA D'ITALIA. - ISSN 0536-0242. - STAMPA. - 61:(2003), pp. 129-144.

Anatomy of carbonate turbidite mega-beds (M. Cassio Formation, Upper Cretaceous, northern Apennines, Italy).

FONTANA, Daniela;
2003

Abstract

Turbidites mega-beds are the product of convulsive sedimentary events and provide time lines for the study of the stratigraphic record. An integrated and detailed study of depositional facies, petrography. paleontology and geochemistry of Cassio mega-beds allows: 1) determination of individual sediment types stored before resedimentation: 2) recognition of source area locations, types of triggering mechanisms, and transport/depositional processes, bottom fauna ecologu and diagenetic modifications.
2003
61
129
144
Anatomy of carbonate turbidite mega-beds (M. Cassio Formation, Upper Cretaceous, northern Apennines, Italy) / Zuffa, G. G.; Fontana, Daniela; Morlotti, E.; PREMOLI SILVA, I.; Sighinolfi, G. P.; Stefani, C. FONTANI L.. - In: MEMORIE DESCRITTIVE DELLA CARTA GEOLOGICA D'ITALIA. - ISSN 0536-0242. - STAMPA. - 61:(2003), pp. 129-144.
Zuffa, G. G.; Fontana, Daniela; Morlotti, E.; PREMOLI SILVA, I.; Sighinolfi, G. P.; Stefani, C. FONTANI L.
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11380/461523
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