J4 ›› 2010, Vol. 40 ›› Issue (2): 321-326.

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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-hui1   

  1. 1.College of Earth Sciences, Jilin University, Changchun 130061|China；
    2.Jilin Horroc Nonferrous Metal Groups Co. Ltd, Panshi, Jilin 132311, China；3.School of Resources &|Environment, Southwest Petroleum University, Chengdu 610500, China
  • Received:2009-05-07 Online:2010-03-26 Published:2010-03-26

Abstract:

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.

Key words: magmatic Cu-Ni sulfide deposit, Hongqiling Jilin Province, Xing’an-Mongolia orogenic belt, geochronology

CLC Number: 

  • P597.3
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