SEDIMENTARY DYNAMICS AND TECTO-VOLCANISM IN THE VENOSA BASIN (BASILICATA, ITALIA)

Direct tecto-volcanism is the main process involved in the sedimentary filling of the Venosa lacustrine basin. Two formations have been distinguished: the Tufarelle Formation and the Piano Regio Formation. In the sedimentary series exposed at the Notarchirico Middle Pleistocene prehistoric site, sev...

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Veröffentlicht in:	Quaternary international 1998-01, Vol.47, p.97-105
Hauptverfasser:	Raynal, J.P., Lefèvre, D., Vernet, G., Pilleyre, T., Sanzelle, S., Fain, J., Miallier, D., Montret, M.
Format:	Artikel
Sprache:	eng
Schlagworte:	Archaeology and Prehistory Earth Sciences Environmental Sciences Global Changes Humanities and Social Sciences Sciences of the Universe Stratigraphy Volcanology
Online-Zugang:	Volltext
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