http://www.cnr.it/ontology/cnr/individuo/prodotto/ID283670
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
- Pagina fine
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#pagineTotali
- 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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