The Tertiary calc-alkaline volcanism of Sardinia affected large areas of Northern and Central part of the Island. This volcanism mainly developed along the main structures of the Sardinian Oligocene-Miocene Rift System, related to a convergent plate margin (Lecca et al., 1997). During the Miocene, a highly explosive phase of the volcanism caused the emplacement of large volumes of prevalently rhyolitic-rhyodacitic pyroclastic flow deposits.

Zeolite mineral exploration in Miocene pyroclastic flow from northwestern Sardinia (Italy). "Zeolite '02" Thessaloniki Greece 2002 / Mameli, A; Naitza, S; Padalino, G; Palomba, M; Rizzo, R; Saviano, Giovanna. - (2002), pp. 218-219. (Intervento presentato al convegno Tessaloniki nel 3-7 June 2002).

Zeolite mineral exploration in Miocene pyroclastic flow from northwestern Sardinia (Italy). "Zeolite '02" Thessaloniki Greece 2002.

SAVIANO, Giovanna
2002

Abstract

The Tertiary calc-alkaline volcanism of Sardinia affected large areas of Northern and Central part of the Island. This volcanism mainly developed along the main structures of the Sardinian Oligocene-Miocene Rift System, related to a convergent plate margin (Lecca et al., 1997). During the Miocene, a highly explosive phase of the volcanism caused the emplacement of large volumes of prevalently rhyolitic-rhyodacitic pyroclastic flow deposits.
File allegati a questo prodotto
Non ci sono file associati a questo prodotto.

I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.

Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11573/194486
 Attenzione

Attenzione! I dati visualizzati non sono stati sottoposti a validazione da parte dell'ateneo

Citazioni
  • ???jsp.display-item.citation.pmc??? ND
  • Scopus ND
  • ???jsp.display-item.citation.isi??? ND
social impact