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    云南雪龙山韧性剪切带中流体包裹体的研究

    孙志明, 李兴振, 沈敢富, 杜德勋, 江新胜

    孙志明, 李兴振, 沈敢富, 杜德勋, 江新胜. 云南雪龙山韧性剪切带中流体包裹体的研究[J]. 沉积与特提斯地质, 2001, 21(3): 82-86.
    引用本文: 孙志明, 李兴振, 沈敢富, 杜德勋, 江新胜. 云南雪龙山韧性剪切带中流体包裹体的研究[J]. 沉积与特提斯地质, 2001, 21(3): 82-86.
    SUN Zhi-ming, LI Xing-zhen, SHEN Gan-fu, DU De-xun, JIANG Xin-sheng. Fluid inclusions from the Xuelongshan ductile shear zone, Yunnan[J]. Sedimentary Geology and Tethyan Geology, 2001, 21(3): 82-86.
    Citation: SUN Zhi-ming, LI Xing-zhen, SHEN Gan-fu, DU De-xun, JIANG Xin-sheng. Fluid inclusions from the Xuelongshan ductile shear zone, Yunnan[J]. Sedimentary Geology and Tethyan Geology, 2001, 21(3): 82-86.

    云南雪龙山韧性剪切带中流体包裹体的研究

    详细信息
    • 中图分类号: P542

    Fluid inclusions from the Xuelongshan ductile shear zone, Yunnan

    • 摘要: 流体包裹体是变质作用及其后期构造作用过程中流体环境中唯一真实客观的记录,对解决某些重要的地质理论问题具有十分重要的意义。对于流体包裹体的形态特征及其成分特征的研究,可反映流体的成因及其演化等问题。
      Abstract: Fluid inclusions tend to objectively record the fluid conditions during the metamorphism and subsequent tectonism. The temperatures and pressures for the fluid inclusion formation are believed to be the significant factors indicating physical and chemical conditions during the fluid inclusion formation. The morphology and compositions of the fluid inclusions from the Xuelongshan ductile shear zone, Yunnan examined in this paper may reflect the genesis, nature and evolution of the fluids from this area. The results of research show that the Xuelongshan ductile shear zone is not only a tectonically deformed zone but also a catathermal and retrogressive metamorphic zone.
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    出版历程
    • 收稿日期:  2001-03-15
    • 发布日期:  2001-09-29

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