Ni-Co-As-Bi minerals in the Silius vein system, (SE Sardinia, Italy): The polymetallic evolution of a word-class fluorspar deposit

被引:0
|
作者
Scano, Ignazio [1 ]
Attardi, Antonio [1 ]
Cocco, Fabrizio [1 ]
Fancello, Dario [1 ]
Murroni, Alessandro [2 ]
Zara, Francesca [1 ]
Naitza, Stefano [1 ]
机构
[1] Univ Cagliari, Dipartimento Sci Chim & Geol, Monserrato, Italy
[2] Mineraria Gerrei Srl, Silius, Italy
关键词
ORE-DEPOSITS; HYDROTHERMAL ACTIVITY; MINERALIZATION;
D O I
暂无
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
The world-class Silius deposit (NE Sardinia, Italy), exploited for decades, represents a huge ENE-WSW to NE-SW directed vein system, characterized by abundant fluorite, minor barite, and Pb-(Zn-Cu-Fe) sulphides in quartz-carbonate gangue. This deposit shows many similarities to other European unconformity-related F-Ba districts linked to the regional-scale event of the breakup of Pangea, such as ore textures, low-temperature high-salinity fluids, and observed mineral assemblages. Besides fluorite, the mineralogy includes other critical raw materials (CRM) such as disseminated tiny LREE minerals and intergrowths of Ni-Co-Fe arsenides-sulpharsenides such as nickeline (NiAs), rammelsbergite (NiAs2), gersdorffite (NiAsS), cobaltite (CoAsS) and arsenopyrite (FeAsS). Ni-Co assemblages, which were recently discovered in this deposit, were investigated by optical microscopy and SEM-EDS.
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页码:96 / 99
页数:4
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