Journal of Jilin University(Earth Science Edition) ›› 2017, Vol. 47 ›› Issue (6): 1763-1783.doi: 10.13278/j.cnki.jjuese.201706114

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Genesis of Amphibolite in Mengdong Group-Complex in Southeastern Yunnan and Its Tectonic Significance

Tan Hongqi1,2, Liu Yuping3   

  1. 1. Institute of Multipurpose Utilization of Mineral Resources, CAGS, Chengdu 610041, China;
    2. College of Earth Science, Chengdu University of Technology, Chengdu 610059, China;
    3. Institute of Geochemistry/State Key Laboratory of Ore Deposit Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China
  • Received:2017-03-06 Online:2017-11-26 Published:2017-11-26
  • Supported by:
    Supported by National Key Basic Research Program of China(G2007CB411408) and National Natural Science Foundation of China(41603034,40972129)

Abstract: Existingin schist and gneiss in Mengdong Group-Complex,the amphibolite belongs to Precambrian Formation in Laojunshan area of southeastern Yunnan, on which metamorphism and deformation superposed. The content of SiO2 ranges from 47.0% to 50.4%. In the discrimination diagrams of Simonen,DF and A-K,it falls in the series of orthometamorphite derived from meta-basite rock. Its geochemical characters show that the total REE contents of amphibolite (w(ΣREE)=(214-267)×10-6) exceed those of oceanic island basalt, while its distribution pattern is similar to that of oceanic island basalt in steep right-dipping with light REE enrichment. The spider diagram shows that it is enriched in Rb,Th,Ta,Nb,Ce and Sm,while depleted of Ba,Zr,Hf and Y, similar to the characteristics of the alkaline basalts within plate. The discrimination diagrams of Zr/TiO2-Nb/Y, TiO2-10MnO-10P2O5,La/10-Nb/8-Y/15,Th/Zr-Nb/Zr,and Th/Hf-Ta/Hf suggest that their protolith should be of alkaline basalt magma series in a continental rift environment. The microstructures of amphibole and plagioclase indicate that the microstructure is relatively free, with free dislocations and dislocation columns, occasionally dislocation rings or dislocation dipoles,which is in accordance with the average pressure and temperature of hornblende-plagioclase minerals of 0.88 GPa and 646℃ respectively, confirming that the highest metamorphic grade is of low amphibolite facies. According to the U-Pb dating of sphenes in plagiogneiss and metamorphic overgrowth zircon in Nanwenhe gneissic granite (230 Ma),the deformation conditions were related to the Indosinian tectono-thermal events, and during this period, the embryo of Laojunshan complex began to form.

Key words: amphibolite, geochemical, tectonic significances, southeastern Yunnan, Mengdong Group-Complex

CLC Number: 

  • P588.3
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