Sedimentary-exalative features in Cu-mineralized sandstones at the base of the Miocene: the example of Pala Mantedda (NW Sardinia, Italy) (Contributo in atti di convegno)

Type
Label
  • Sedimentary-exalative features in Cu-mineralized sandstones at the base of the Miocene: the example of Pala Mantedda (NW Sardinia, Italy) (Contributo in atti di convegno) (literal)
Anno
  • 2004-01-01T00:00:00+01:00 (literal)
Alternative label
  • S. Fadda, M. Fiori, C. Matzuzzi, S. Pretti (2004)
    Sedimentary-exalative features in Cu-mineralized sandstones at the base of the Miocene: the example of Pala Mantedda (NW Sardinia, Italy)
    in The Interim IAGOD Conference on Metallogeny of the Pacific Northwest: Tectonics, Magmatism and Metallogeny of Active Continental Margins, Vladivostok, Russia, 1 - 20 september 2004
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • S. Fadda, M. Fiori, C. Matzuzzi, S. Pretti (literal)
Pagina inizio
  • 419 (literal)
Pagina fine
  • 422 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#pagineTotali
  • 4 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • IGAG-CNR, Istituto di Geologia Ambientale e Geoingegneria, UOS di Cagliari, DIGITA - Università di Cagliari, Piazza D'Armi 09100 Cagliari (literal)
Titolo
  • Sedimentary-exalative features in Cu-mineralized sandstones at the base of the Miocene: the example of Pala Mantedda (NW Sardinia, Italy) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#isbn
  • 5-8044-0470-9 (literal)
Abstract
  • Prospecting in the northern part of Sardinia, within a N-S-trending tectonic trough has led to the discovery of a number of mineralized sections in the terrigenous sediments that were produced during a Miocene marine transgression. The mineralization occurs at the contact between pyroclastics and clastic sediments and consists of sulphide phases in chalcedony representing the surficial deposition of exhalative fluids connected to the Tertiary volcanism. The source of metals was probably of both hydrothermal and sinsedimentary origin. (literal)
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