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    中国百强科技报刊

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    Volume 43 Issue 5
    May  2018
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    Wang Yin, Liu Hailing, Zhang Xuefen, Shen Baoyun, Zhu Rongwei, Zhou Yang, 2018. Developmental Stage and Formation Mechanism of Nanoparticles in Xiaomei Ductile Shear Zone on Hainan Island. Earth Science, 43(5): 1532-1541. doi: 10.3799/dqkx.2017.540
    Citation: Wang Yin, Liu Hailing, Zhang Xuefen, Shen Baoyun, Zhu Rongwei, Zhou Yang, 2018. Developmental Stage and Formation Mechanism of Nanoparticles in Xiaomei Ductile Shear Zone on Hainan Island. Earth Science, 43(5): 1532-1541. doi: 10.3799/dqkx.2017.540

    Developmental Stage and Formation Mechanism of Nanoparticles in Xiaomei Ductile Shear Zone on Hainan Island

    doi: 10.3799/dqkx.2017.540
    • Received Date: 2017-03-30
    • Publish Date: 2018-05-15
    • In order to investigate the development process and formation mechanism of nanoparticles in ductile shear zone, three types of rocks were sampled from the Xiaomei ductile shear zone on Hainan island, including granite, granitic gneiss and quartz schist. And the morphology of the nanoparticles was observed by scanning electron microscope (SEM). The results show that there are two kinds of basic forms of nanoparticles:spherical and columnar, and the nanoparticles (nanograins) are widely developed in all three kinds of rocks. The nanoparticles (nanorods) in granite gneiss are most developed. The aggregated morphology of nanoparticles indicates that the development can be divided into three stages including granulation, alienation and stratification accumulation. The second phase of activity starts with the activation stage which forms complex-nanoparticles, and then repeats the above stage. Combined with the morphological changes of nanoparticles, it is concluded that the formation mechanism is probably brittle-ductile deformation.

       

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