Fluid regime and ore formation in the tungsten(–yttrium) deposits of Kyzyltau (Mongolian Altai): evidence for fluid variability in tungsten–tin ore systems

Author:

Graupner T,Kempe U,Dombon E,Pätzold O,Leeder O,Spooner E.T.C

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference87 articles.

1. Redox conditions of formation of tin–ore mineralization zones of various productivity;Bannikova;Geokhimiya,1989

2. Barabanov, V.F., 1985. Geokhimiya. Leningrad, Nedra, 423 pp., in Russian.

3. Investigation of the composition of fluid inclusions in minerals with the cryometric method;Borisenko;Geologiya i Geofizika,1977

4. The composition of a primary granite-derived ore fluid from SW England, determined by fluid inclusion analysis;Bottrell;Geochim. Cosmochim. Acta,1988

5. Calculation of the thermodynamic and geochemical consequences of non-ideal mixing in the system H2O–CO2–NaCl on phase relations in geologic systems: equation of state for H2O–CO2–NaCl fluids at high pressures and temperatures;Bowers;Geochim. Cosmochim. Acta,1983

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