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June 01, 1995
P-V-T-X -fO 2 evolution from wolframite to sulphide depositional stages in intragranitic W-veins; an example from the Spanish Central System
Elena Vindel;
Elena Vindel
Universidad Complutense, Departamento de Cristalografia y Mineralogia, Madrid, Spain
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European Journal of Mineralogy (1995) 7 (3): 675–688.
Article history
first online:
02 Mar 2017
Citation
Elena Vindel, Jose Angel Lopez, Marie-Christine Boiron, Michel Cathelineau, Angel Carmelo Prieto; P-V-T-X -fO 2 evolution from wolframite to sulphide depositional stages in intragranitic W-veins; an example from the Spanish Central System. European Journal of Mineralogy ; 7 (3): 675–688. doi:
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Index Terms/Descriptors
- alteration
- concentration
- Europe
- fluid inclusions
- granites
- hydrothermal alteration
- hydrothermal processes
- Iberian Peninsula
- igneous rocks
- inclusions
- metal ores
- metasomatism
- mineral deposits, genesis
- ore-forming fluids
- P-T conditions
- peraluminous composition
- plutonic rocks
- quartz veins
- salinity
- Southern Europe
- Spain
- Spanish Central System
- sulfides
- tungstates
- tungsten ores
- veins
- volatiles
- wolframite
Latitude & Longitude