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《Journal of Jilin University(Earth Science Edition)》 2010-02
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Mineralization Age of the No.3 Ore-bearing Intrusion and Its Petrological Significance in Hongqiling Cu-Ni Sulfide Deposits,Jilin Province

LIU Jin-yu1,2,XI Ai-hua1,3,GE Yu-hui3,SUN Hong-tao2,GONG Peng-hui11.College of Earth Sciences,Jilin University,Changchun 130061,China2.Jilin Horroc Nonferrous Metal Groups Co.Ltd,Panshi,Jilin 132311,China3.School of Resources & Environment,Southwest Petroleum University,Chengdu 610500,China  
The Hongqiling magmatic Cu-Ni sulfide deposit represented by No.1 and No.7 intrusions belongs to a typical magmatic liquation deposit in Xing'an-Mongolia orogenic belt.More than 30 mafic-ultramafic intrusions have been found in the Hongqiling mining district.The No.3 intrusion,whose geological occurrence were different from those of other ore-bearing rock bodies,was once thought to be formed during the Yanshanian era.The 40Ar/39Ar isotopic dating of amphiboles collected from different depths of core samples in No.3 intrusion gave a(228.2±3.0) Ma plateau age and a(230.1±7.1) Ma isochron age.These isotopic ages consist generally with the ages of No.1 intrusion published before,all being derived from the Early Indosinian magmatism.Geochemical studies of No.1,No.3,and No.7 ore-bearing intrusions also suggest these intrusions were derived from a common source according to their similar curve patterns of REE and trace elements.This opinion could be significant for guiding further exploration of the magmatic Cu-Ni deposits in the area.
【Fund】: 国家自然科学基金项目(40572058);; 四川省教育厅自然科学类项目(省504);; 四川省重点学科建设项目(SZD414)
【CateGory Index】: P597.3
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