Journal of Jilin University(Earth Science Edition) ›› 2019, Vol. 49 ›› Issue (3): 690-708.doi: 10.13278/j.cnki.jjuese.20180240

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Geochronology, Geochemistry and Tectonic Implications of Early Silurian Intermediate-Acid Intrusive Rocks in East of Jueluotage Belt, Eastern Tianshan

Yu Jielu1, Yu Jiejiang1, Yang Wanzhi2, Zhang Yuanhou1, Guo Xiuwei1   

  1. 1. College of Earth Sciences, Jilin University, Changchun 130061, China;
    2. Xinjiang Institute of Geological Survey, Urumqi 830000, China
  • Received:2018-09-14 Online:2019-06-03 Published:2019-06-03
  • Supported by:
    Supported by National Natural Science Foundation of China (41672050) and Project of the Xinjiang Uygur Autonomous Region Geological Survey Fund Management Center (Y14-5-LQ05)

Abstract: In order to ascertain the formation age, source and tectonic properties of the intermediate-acid intrusive rocks in the Yuhai area of the eastern Jueluotage belt in the eastern Tianshan, this paper systematically presents LA-ICP-MS zircon U-Pb geochronology, whole rock geochemistry and Sr-Nd isotopes data of the rocks in this area. The selected zircons of two samples show obvious oscillation zoning in cathodoluminescence (CL) images, and have Th/U value of 0.28-0.59, indicating a magmatic origin. The zircon U-Pb dates indicate that they formed in the Early Silurian of (433.2-431.2) Ma, representing the emplacement age of these host rocks. These samples have w(SiO2)=57.88%-69.01%,w(Na2O)=3.46%-5.07%,w(K2O)=0.50%-1.65%,Na2O/K2O=4.26-6.79,Mg#=45.1-52.3,and A/CNK=0.89-1.00; the rare earth element distribution patterns are right-slipped, LREE/HREE=5.55-11.47,(La/Yb)N=4.18-13.54,and δEu=0.82-1.25;the trace element spider diagrams show that they are enriched in LILE (Ba, U, K and Sr), moderately depleted of HFSE (Th, Ti, Nb and Ta); the value of εNd(t) of the whole rock is between 6.1 and 7.0. The study shows that the magma source of the intermediate-acid intrusive rocks in the Early Silurian is mainly young crustal material. Combining with the characteristics of igneous rock association, magmatism and regional tectonic evolution history, it is considered that the intermediate-acid intrusive rocks of the Early Silurian were formed in the active continental margin environment under the northward subduction of the Kanggur Ocean plate (Turpan-Hami block). Thus, the time of the Kanggur plate subduction can be traced back to the Early Silurian.

Key words: eastern part of Jueluotage belt, Eastern Tianshan, Early Silurian, intermediate-acid intrusive rocks, geochronology, geochemistry, tectonic implications

CLC Number: 

  • P588.12
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