In this work a report is given of the geological, petrographic and ore mineralogical features of several sulphide-bearing quartz breccia (SQB) bodies outcropping in a structurally complex sector of the Orobic Alps (Southern Alpine Domain) and close to the uranium-rich mining area of Novazza. Although little studied, these breccia bodies were previously attributed to different genetic processes and/or geological domains (e.g., Crystalline Basement, Basal Conglomerate formation). The features of the SQB bodies suggest a hydrothermal origin likely related to the large-scale hydrothermal process causing the formation of the nearby uranium ore deposit at Novazza.

Phreatic sulphide bearing quatz breccias between cristalline basement and Collio Formation (Southern Alps, Italy) / D. Servida, L. De Capitani, G. Grieco, M. Moroni, D. Ravagnani, F. Rodeghiero, I. Venerandi. - In: ITALIAN JOURNAL OF GEOSCIENCES. - ISSN 2038-1719. - 129:2(2010), pp. 223-236. [10.3301/IJG.2010.03]

Phreatic sulphide bearing quatz breccias between cristalline basement and Collio Formation (Southern Alps, Italy)

L. De Capitani;G. Grieco;M. Moroni;
2010

Abstract

In this work a report is given of the geological, petrographic and ore mineralogical features of several sulphide-bearing quartz breccia (SQB) bodies outcropping in a structurally complex sector of the Orobic Alps (Southern Alpine Domain) and close to the uranium-rich mining area of Novazza. Although little studied, these breccia bodies were previously attributed to different genetic processes and/or geological domains (e.g., Crystalline Basement, Basal Conglomerate formation). The features of the SQB bodies suggest a hydrothermal origin likely related to the large-scale hydrothermal process causing the formation of the nearby uranium ore deposit at Novazza.
Phreatic breccia; hydrothermal activity; Orobic Alps; Novazza; quartz; sulphides
Settore GEO/09 - Georisorse Miner.Appl.Mineral.-Petrogr.per l'amb.e i Beni Cul
Settore GEO/08 - Geochimica e Vulcanologia
Settore GEO/06 - Mineralogia
2010
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/2434/151099
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