Estudio de inclusiones fluidas en la mineralización de wolframio de Garganta de los Montes (Sistema Central)
- Encarnacion Quilez Valdelvira
- J. Sierra López 1
- Elena Vindel Catena
- 1 Universidad Complutense de Madrid (Facultad de Ciencias Geológicas. Departamento de Cristalografía y Mineralogía)
ISSN: 0210-6558
Datum der Publikation: 1988
Ausgabe: 11
Nummer: 2
Seiten: 105-108
Art: Artikel
Andere Publikationen in: Boletín de la Sociedad Española de Mineralogía
Zusammenfassung
The W mineralizations of Garganta de los Montes (Spanish Central System) is emplaced in a series of migmatized gneisses and seems to be spatially and genetically related to the La Cabrera granitoid. CO2-H2O fluid inclusions, water-rich, and water-rich with different cations, have been recognized in quartz .The dilution of the carbonic-water-rich fluids, and the consequent altering of the chemical and physical characteristics of the mineralizing system, make the W-bearing complexes unstable, which wo ul d have induced W precipitation.