Origin of mineralizing fluids of the sediment-hosted navachab gold mine, Namibia: Constraints from stable (O, H, C, S) isotopes

Economic Geology

Volumn 105, Issue 2, 2010, Pages 285-302

  Wulff, Katharina ^a   Dziggel, Annika ^a   Kolb, Jochen ^b   Vennemann, Torsten ^c   Böttcher, Michael E ^d   Michael Meyer, F ^a  

^a RWTH AACHEN UNIVERSITY   (Germany)

^b GEOLOGICAL SURVEY OF DENMARK AND GREENLAND   (Denmark)

^c UNIVERSITY OF LAUSANNE   (Switzerland)

^d LEIBNIZ INSTITUTE FOR BALTIC SEA RESEARCH   (Germany)

Author keywords

[No Author keywords available]

Indexed keywords

BISMUTH TELLURIDE; BISMUTHINITE; CARBONATE CONTENT; CLINOPYROXENES; FLUID-ROCK INTERACTION; GEOTHERMAL GRADIENTS; HYDRAULIC REGIMES; IGNEOUS ACTIVITY; ISOTOPIC FRACTIONATIONS; LAMPROPHYRE; MAGMATIC FLUIDS; METAMORPHIC CONDITIONS; METAMORPHIC FLUIDS; METAPELITES; METASEDIMENTARY ROCKS; MINERALIZING FLUIDS; NAMIBIA; PHYSICOCHEMICAL CONDITIONS; POLYMETALLIC; STEEP GRADIENTS; TOTAL VARIATION;

BISMUTH; CARBONATE MINERALS; COPPER COMPOUNDS; FLUIDS; GOLD; GOLD MINES; IGNEOUS ROCKS; IRON ORES; ISOTOPES; MARBLE; MICA; QUARTZ; ROCKS; SILICATE MINERALS; TELLURIUM COMPOUNDS; ZINC SULFIDE;

LEAKAGE (FLUID);

BIOTITE; CARBONATE GROUP; DIKE; FLUID FLOW; FLUID-STRUCTURE INTERACTION; GOLD MINE; GRANITE; HEAVY METAL; ISOTOPIC FRACTIONATION; LAMPROPHYRE; MAGMATISM; MARBLE; METAMORPHIC ROCK; METAMORPHISM; MINERALIZATION; PHYSICOCHEMICAL PROPERTY; QUARTZ; SEDIMENTARY ROCK; STABLE ISOTOPE;

DAMARA BELT; NAMIBIA;

EID: 78149295594     PISSN: 03610128     EISSN: None     Source Type: Journal    
DOI: 10.2113/gsecongeo.105.2.285     Document Type: Article

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