Effects of magmatic processes, serpentinization, and talc-carbonate alteration on sulfide mineralogy and ore textures in the black swan disseminated nickel sulfide deposit, yilgarn craton

Economic Geology

Volumn 104, Issue 4, 2009, Pages 539-562

  Barnes, Stephen J ^a   Wells, Martin A ^a   Verrall, Michael R ^a  

^a CSIRO   (Australia)

Author keywords

[No Author keywords available]

Indexed keywords

ANTIGORITE; CARBONATE CONTENT; CARBONATED SERPENTINITE; DISTINCTIVE FEATURES; EXSOLUTION; GANGUE MINERALS; HALOGEN CONTENTS; INTER-GROWTHS; INTERGROWTH; KOMATIITE; LIZARDITE; MAGMATIC PROCESS; MICRO BEAMS; NICKEL SULFIDE; SEA FLOOR; SEGREGATION VESICLES; SERPENTINITE; SERPENTINIZATION; SULFIDE MELT; THERMAL METAMORPHISM; ULTRAMAFIC CUMULATE; VOLUME EXPANSION; WESTERN AUSTRALIA;

CARBONATE MINERALS; CHROMITE; CHROMITE DEPOSITS; CRYSTALLOGRAPHY; DEPOSITS; KAOLINITE; MAGNETITE; MINERALS; NICKEL; OLIVINE; OXIDE MINERALS; OXYGEN; PYRITES; RAMAN SPECTROSCOPY; SEGREGATION (METALLOGRAPHY); SERPENTINE; SILICATE MINERALS; TALC; TEXTURES; UNDERWATER MINERALOGY;

CARBONATION;

CARBONATE; KOMATIITE; MAGMATISM; MINERALOGY; SERPENTINIZATION; SULFIDE; TALC;

CYGNUS ATRATUS;

EID: 68649122611     PISSN: 03610128     EISSN: None     Source Type: Journal    
DOI: 10.2113/gsecongeo.104.4.539     Document Type: Article

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