Along the thalweg of the Torrente Tiepido, outcrops a sedimentary succession of the Pleistocene, about 750m thick. For the first 605m the succession is composed of clayey-silt and sandy sediments deposited in a marine environment. For the remaining 145m it is composed of gravels, clayey-silt sands and peaty clays from a prevalently continental environment. The age of the succession, based on the study of Foraminifera from the marine section of the series, is lower Pleistocene; the age of the continental part is between the lower Pleistocene and the Mindel-Riss interglacial. -from English summary

La successione Pleistocenica marina e continentale del t. Tiepido / A. Annovi, M. Cremaschi, P. Fregni, G. Gasperi. - In: GEOGRAFIA FISICA E DINAMICA QUATERNARIA. - ISSN 0391-9838. - 2:1(1979), pp. 1-22.

La successione Pleistocenica marina e continentale del t. Tiepido

M. Cremaschi
Secondo
;
1979

Abstract

Along the thalweg of the Torrente Tiepido, outcrops a sedimentary succession of the Pleistocene, about 750m thick. For the first 605m the succession is composed of clayey-silt and sandy sediments deposited in a marine environment. For the remaining 145m it is composed of gravels, clayey-silt sands and peaty clays from a prevalently continental environment. The age of the succession, based on the study of Foraminifera from the marine section of the series, is lower Pleistocene; the age of the continental part is between the lower Pleistocene and the Mindel-Riss interglacial. -from English summary
margine appenninico, facies continentali, stratigrafia del quaternario
Settore GEO/01 - Paleontologia e Paleoecologia
Settore GEO/04 - Geografia Fisica e Geomorfologia
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Utilizza questo identificativo per citare o creare un link a questo documento: http://hdl.handle.net/2434/176985
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