EVOLUTION AND METALLOGENESIS OF ULTRABASIC MAGMA OF JINBAOSHAN PT-PD DEPOSIT,MIDU
Yang Zong
Abstract
Yang Zong
Abstract
The Jinbaoshan Pt-Pd deposit is the largest independent Pt family deposit discovered in recent years.It belongs to the Pt-Pd deposit of Cu-Ni sulfide type of ultrabasic rock body.The earlier immiscible separation of deep sulfide is the main controlling factor of metallogenesis of Jinbaoshan Pt family deposit.It is generally serpentinized in the posterior stage of high T fluid activity.The concentration place of metallic sulfide is just the position of Pt-Pd metallogenesis.The metallic sulfide is an indirect ore-prospecting guide in the Fe Ultrabasic rock.
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The Jinbaoshan Pt-Pd deposit is the largest independent Pt family deposit discovered in recent years.It belongs to the Pt-Pd deposit of Cu-Ni sulfide type of ultrabasic rock body.The earlier immiscible separation of deep sulfide is the main controlling factor of metallogenesis of Jinbaoshan Pt family deposit.It is generally serpentinized in the posterior stage of high T fluid activity.The concentration place of metallic sulfide is just the position of Pt-Pd metallogenesis.The metallic sulfide is an indirect ore-prospecting guide in the Fe Ultrabasic rock.
Key concepts: Ultramafic rock, Sulfide, Geology, Geochemistry, Prospecting, Volcanogenic massive sulfide ore deposit, Magma, Mineralogy