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The Experimental Study of Talc and Antigorite Evolution under Dry-Thermal Condition
  • ISSN号:1000-4734
  • 期刊名称:《矿物学报》
  • 时间:0
  • 分类:P579[天文地球—矿物学;天文地球—地质学]
  • 作者机构:[1]College of Resources and Civil Engineering,Northeastern University
  • 相关基金:Supported by National Natural Science Foundation (Grant No.:40872045; 41172047);The Opening Project of Key Laboratory of Solid Waste Treatment and Resource Recycle (SWUST), Ministry of Education (12zxgk01)
中文摘要:

The Xiuyan Jade samples were treated under thermal conditions. By polarizing microscope, the three kinds of jade were choosed. With DTA-TG analysis, three transition temperatures were obtained which were 600℃, 770℃ and 840℃. The study interpreted the mechanism of Xiuyan Jade under thermal condition through XRD analysis results. The mechanism of antigorite thermal activation was as following: when the temperature reached 600℃, the hydroxyl in octahedral sheet began dehydrating, and the new mineral phase forsterite was found, but the layer structure was maintained; when the temperature reached 770℃, the layer structure of antigorite was destroyed; when the temperature reached 840℃, the crystallinity of forsterite was improved, then another new mineral phase enstatite appeard. For talc, it was likely turn to enstatite directly while the temperature rising, and the appearance of SiO2 was most likely due to the conversion of talc.

英文摘要:

The Xiuyan Jade samples were treated under thermal conditions. By polarizing microscope, the three kinds of jade were choosed. With DTA-TG analysis, three transition temperatures were obtained which were 600℃, 770℃ and 840℃. The study interpreted the mechanism of Xiuyan Jade under thermal condition through XRD analysis results. The mechanism of antigorite thermal activation was as following: when the temperature reached 600℃, the hydroxyl in octahedral sheet began dehydrating, and the new mineral phase forsterite was found, but the layer structure was maintained; when the temperature reached 770℃, the layer structure of antigorite was destroyed; when the temperature reached 840℃, the crystallinity of forsterite was improved, then another new mineral phase enstatite appeard. For talc, it was likely turn to enstatite directly while the temperature rising, and the appearance of SiO2 was most likely due to the conversion of talc.

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期刊信息
  • 《矿物学报》
  • 中国科技核心期刊
  • 主管单位:中国科学院
  • 主办单位:中国科学院地球化学研究所 中国矿物岩石地球化学学会
  • 主编:胡瑞忠
  • 地址:贵州省贵阳市观山湖区林城西路99号
  • 邮编:550081
  • 邮箱:kwxb@ms.gyig.ac.cn
  • 电话:0851-5891352
  • 国际标准刊号:ISSN:1000-4734
  • 国内统一刊号:ISSN:52-1045/P
  • 邮发代号:66-17
  • 获奖情况:
  • 国内外数据库收录:
  • 被引量:10998