RT Journal Article
T1 Comportamiento del nitrógeno en los procesos mineralizadores de los yacimientos de Sb de Mari Rosa y El Juncalón (Zona Centro Ibérica)
T1 Nitrogen beha viour during ore-forming processes at Mari Rosa and El Juncalón Sb-deposits (Central Iberían zone)
A1 Ortega, Lorena
AB Fluid inclusions associated to Mari Rosa and El Juncalón antimony deposits show that N2 is a relevant component of the fluid phase. Besides, altered host rocks show significant enrichment in nitrogen rather than depletion. N2 in hydrothermal fluids mainly originates from the release to the fluid of ammonium from NHJj- bearing silicates at T>550-600°C (Hallam & Eugster, 7 976; Dubessy & Ramboz, 7 986). According to that, inner contact metamorphic aureoles around near-by granitic bodies were the probable sites for nitrogen hydrothermal lixiviation
PB Sociedad Geológica de España
YR 1994
FD 1994
LK http://hdl.handle.net/10272/13931
UL http://hdl.handle.net/10272/13931
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 1 jun 2026