The application of capillary ion analysis to the geochemistry of natural aqueous fluids and in particular to the analysis of fluid inclusions in minerals
Por: Hallbauer, Dieter Klaus
.
Tipo de material: 
Articulo de congreso Editor: Utrecht: VSP BV, 1997Descripción: pp. 409-424 ilus.Tema(s): ELECTROFORESIS | GEOQUÍMICA | INCLUSIONES FLUIDAS | SOLUCIONES ACUOSASClasificación CDU: R/061.3:55(100)/C74/30/9|25
En: International Geological Congress, 30 Pei, Rongfu, Proceedings of the 30th International Geological Congress, vol. 9: Energy and mineral resources for the 21st century; geology of mineral deposits, mineral economics, 1997
| Tipo de ítem | Ubicación actual | Signatura | Estado | Fecha de vencimiento | Código de barras |
|---|---|---|---|---|---|
Articulo de congreso
|
Biblioteca INGEMMET | R/061.3:55(100)/C74/30/9|25 (Navegar estantería) | Disponible | 34870 | |
Congreso
|
Biblioteca INGEMMET | R/061.3:55(100)/C74/30/9 (Navegar estantería) | Disponible | 29223 |
Navegando Biblioteca INGEMMET Estantes Cerrar el navegador de estanterías
| R/061.3:55(100)/C74/30/9|22 Significance of organic matter and paleoenvironment for formation of the early Sinian manganese carbonate ore deposits in Yangtze platform | R/061.3:55(100)/C74/30/9|23 Siliceous, high-magnesian parental magma compositions of the PGE-rich early paleoproterozoic layered intrusion belt of northern Finland | R/061.3:55(100)/C74/30/9|24 Some major mineral deposits in China: their tectonic setting and deposit model characteristics | R/061.3:55(100)/C74/30/9|25 The application of capillary ion analysis to the geochemistry of natural aqueous fluids and in particular to the analysis of fluid inclusions in minerals | R/061.3:55(100)/C74/30/9|26 The metasomatic hydrothermal metallogeny | R/061.3:55(100)/C74/30/9|27 The model of gaseous and ionic haloes of inclusions in gold deposit | R/061.3:55(100)/C74/30/9|28 The model of uranium mineralization in discharge areas (depressurization areas) of fossil hydrothermal systems |
No hay comentarios para este ejemplar.