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- W2381684662 abstract "The Xiangshan Cu-Ni sulfide deposit is a multiple ore-bearing intrusion and composes of gabbro,pyroxene peridotite,aplitic gabbro and Ti-Fe gabbro,which is located in the centre segment of Tudun-Tulaergen mafic-ultramafic rock belt,the northern of the East Tianshan,and controlled by the Kangurtag-Huangshan ductile sheer zone.The rocks and ores in Xiangshan Cu-Ni deposit,with similar mantle-normalizaed PGE patterns and fractionation between PPGE and IPGE,which range from 0.74×10-9-2.82×10-9 and 20.64×10-9-148.99×10-9 in ∑ PGE respectively.The initial magma of Xiangshan Cu-Ni deposit is high MgO(≥4.97%) and undepleted PGE,which originated from the depleted mantle.But the parental magma is visibly depleted in PGE,possibly due to sulfide immiscibility during the ascent and the main factors include crustal contamination and fractionation of olivine,pyroxene and plagioclase." @default.
- W2381684662 created "2016-06-24" @default.
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- W2381684662 date "2013-01-01" @default.
- W2381684662 modified "2023-09-26" @default.
- W2381684662 title "Platinum Group Elements Geochemistry and Its Implication for the Xiangshan Cu-Ni Sulfide Deposit,East Tianshan,China" @default.
- W2381684662 hasPublicationYear "2013" @default.
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