Authigenic Cu-carbonates in sandstones at he base of Miocene in the Logudoro Region (NW Sardinia, Italy) (Contributo in atti di convegno)

Type
Label
  • Authigenic Cu-carbonates in sandstones at he base of Miocene in the Logudoro Region (NW Sardinia, Italy) (Contributo in atti di convegno) (literal)
Anno
  • 2003-01-01T00:00:00+01:00 (literal)
Alternative label
  • Fadda S., Fiori M., Matzuzzi C. (2003)
    Authigenic Cu-carbonates in sandstones at he base of Miocene in the Logudoro Region (NW Sardinia, Italy)
    in Seventh Biennal SGA Meeting "Mineral Exploration and Sustainable Development", Atene, 24-28 august 2003
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Fadda S., Fiori M., Matzuzzi C. (literal)
Pagina inizio
  • 669 (literal)
Pagina fine
  • 672 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#note
  • Proceed. Vol. 2 pp 669-672 ISBN 90 5966015 3 (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 (literal)
Titolo
  • Authigenic Cu-carbonates in sandstones at he base of Miocene in the Logudoro Region (NW Sardinia, Italy) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#isbn
  • 90-5966-015-3 (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 bottom terrigenous sediments that were produced during a Miocene marine transgression. The mineralization occurs at the contact between pyroclastics and clastic sediments and consists of authigenic oxides and sulphides, suggesting fluctuations of redox conditions in a near-shore, high-pH environment. Evidence indicates that metals were transported under warm and semi-arid climatic conditions by ground waters and deposited in environments characterized by high pH and fluctuating Eh conditions. Evidence also suggests that mineralization occurred during diagenesis. (literal)
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