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- W860202181 abstract "Received 6 December 2010,accepted 4 January 2011 Abstract: The Wadi Bayhan mafic-ultramafic intrusions associated with magmatic PGE-bearing Cu-Ni sulphide deposit are located in the south margin of the Arabian-Nubian Shield,SW Yemen. The intrusions consist of dunite,olivine-pyroxenite,lherzolite,hornblendite,gabbro and gabbronorite. The dunite and lherzolite are the main host rock for the Cu-Ni ores. The new data of the chemical compositions of the rocks have SiO2 ( 50% 53. 6% ) ,Al2O3 ( 0-32% ) and MgO ( 4% -28% ) ,and relatively low TiO2 ( 0-3. 2% ) and K2 O + Na2O ( 0. 04% 5. 2% ) . The geochemical characteristics indicate that the parental magma is high-magnesium tholeiitic. Sulfur had reached saturation and immiscible sulfides droplets segregated from silicate magmas before their emplacement." @default.
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- W860202181 date "2011-01-01" @default.
- W860202181 modified "2023-09-27" @default.
- W860202181 title "Geochemistry and genesis of magmatic PGE-bearing Cu-Ni sulphide deposit in Wadi Bayhan, southeastern Yemen" @default.
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