Journal of Jilin University(Earth Science Edition) ›› 2015, Vol. 45 ›› Issue (2): 364-373.doi: 10.13278/j.cnki.jjuese.201502103

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Neo-Archaean Magmatic Event in Erguna Massif of Northeast China: Evidence from the Zircon LA-ICP-MS Dating of the Gneissic Monzogranite from the Drill

Shao Jun, Li Yongfei, Zhou Yongheng, Wang Hongbo, Zhang Jing   

  1. Shenyang Institute of Geology and Mineral Resources/Shenyang Center of Geological Survey, China Geological Survey, Shenyang 110034, China
  • Received:2014-07-12 Published:2015-03-26

Abstract:

The nature and age of the basement of Erguna massif had long been a geological controversy. The zircon LA-ICP-MS dating of the Gneissic monozgranite from the drill (No.ZK6301, Depth: 226 m) of the Pb-Zn polymetallic deposit in Biliya, southwestern Derbugan county has been conducted. The results yield 4 different groups of concordant age: 2 549-2 562 Ma(weighted-mean age:(2 555±19) Ma,MSWD=0.17,n=3),2 596-2 624 Ma(weighted-mean age(2 606±17) Ma,MSWD=0.032,n=17),2 688-2 715 Ma(weighted-mean age(2 702±18) Ma, MSWD=0.70,n=3),2 786 Ma(n=1). Their zircon U-Pb dating plots (24 out of 29 plots) show a remarkable consistence. Based on the zircon spot analysis for its Th,U content and Th/U ratios, the 207Pb/206Pb age of 2 549-2 562 Ma implies a late tectono-thermal event; and the weighted-mean age 2 606±17 Ma (MSWD=0.032,n=17) reflects the crystallization age in corresponding to the period of Neo-Archaean.In connection with the previous studies, the old basement of Erguna massif probably widely distributes in the south and north region. This suggests a far south extension of this massif beyond Derbugan fault. This can help to understand the palinspastic reconstruction for the eastern part of the Central Asian Orogenic Belt(CAOB).

Key words: Erguna massif, gneissic monzogranite, zircon U-Pb dating, Neo-Proterozoic, Derbugan fault, Biliya Pb-Zn polymetallic deposit

CLC Number: 

  • P588.12

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