Bismuth Minerals in the Molibdenum Showings from Salto di Quirra District, SE Sardinia, Italy (Contributo in atti di convegno)

Type
Label
  • Bismuth Minerals in the Molibdenum Showings from Salto di Quirra District, SE Sardinia, Italy (Contributo in atti di convegno) (literal)
Anno
  • 2013-01-01T00:00:00+01:00 (literal)
Alternative label
  • S. Fadda, M. Fiori (2013)
    Bismuth Minerals in the Molibdenum Showings from Salto di Quirra District, SE Sardinia, Italy
    in 23° INTERNATIONAL MINING CONGRESS AND EXIBITION OF TURKEY, ANTALYA - TURKEY, Antalya TURKEY, 16-19 April 2013
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • S. Fadda, M. Fiori (literal)
Pagina inizio
  • 2009 (literal)
Pagina fine
  • 2019 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#pagineTotali
  • 11 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • IGAG - CNR, Istituto di Geologia Ambientale e Geoingegneria (literal)
Titolo
  • Bismuth Minerals in the Molibdenum Showings from Salto di Quirra District, SE Sardinia, Italy (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#isbn
  • 978-605-01-0467-7 (literal)
Abstract
  • The mineralizations related to the Hercynian magmatism of Sardinia are represented by interesting ore-associations. Molybdenum is scattered in several part of the island and many Mo prospects are Known in the Ogliastra region, SE Sardinia where the molybdenite-wolframite vein of Perda Majori displays mineralogical peculiarities of extreme rareness. A member of the lillianite-gustavite series has been detected and the samples compared with data collected from the literature. In the system PbS-Ag2S-Bi2S3 most of our samples spread between the line lollianite-gustavite join. The possible occurrence of solid solutions having compositions along both these joins is suggested in litterature but there is a miscibility gap in the series at temperatures above 500°C. High-temperature natural phases belonging to the lillianite-like structures situated in the compositional gaps should commonly exibit exsolution phenomena. The exsolved textures of Pb-Ag-Bi sulphosalts from Perda Majori let the mineralization under study be referred to pneumatholitic-hydrothermal stages of deposition. (literal)
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