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断层泥伊利石物理化学特征及其意义

Characteristics of Illite Minerals in Fault Gouge and Their Geological Implications

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【作者】 张秉良周永胜袁仁茂李康

【Author】 Zhang Bingliang;Zhou Yongsheng;Yuan Renmao;Li Kang;Institute of Geology,CEA;

【机构】 中国地震局地质研究所

【摘要】 通过X射线衍射和化学分析等方法,研究了云南水电站断层泥中伊利石物理化学特征,结果显示:1伊利石物质的X射线衍射特征为Δ[(002)-(001)]>8,Ir>1,BB1<4°,属I+ISII有序混层,膨胀层小于15%,晶胞参数b0=8.991,1M多型结构;2K2O的平均含量9.1%变化范围在8.5%-10%之间;3K2O和Fe2O3含量之间为负相关,K2O含量与Δ[(002)-(001)]2θ值呈正相关,而K2O与Ir值呈负相关。上述特征表明该断层泥伊利石是在低温(小于200℃)低压环境下生成。它的形成与断层稳定滑动机制有关。由此推测该断层未来发生大地震的可能性较小。

【Abstract】 The characteristics of minerals,such as illite,etc.in fault gouge from Xiaowan Fault are studied with X-ray diffraction and chemical analysis. The results show that :( 1) X-ray diffraction features of illite are?[(002)?(001)]>8?,Ir>1,BB1 <4?,belonging to orderly mixed layer.Expansive layer accounts are smaller than 15%.The crystal cell parameters b0=8.991 ?,1M polytype structure.(2)KO2 content varies from 4.18%to 5.56%.( 3) There is negative correlation exists between K2 O and Fe2O3. There is a positive correlation between ?[(002)?(001)]and K2 O,but negative correlation exists between K2 O and Ir. All of characteristics suggest that illite was formed in the environment with low-temperature and low-pressure,which is related with the low level of fault activity and low probability of strong earthquake occurrence in future.

【关键词】 断层泥伊利石X射线衍射化学分析
【Key words】 Fault gougeIlliteX-ray diffractionChemical analysis
【基金】 国家自然科学基金(批准号:41172193,40572127,49772168);中国地震局地质研究所基本科研业务专项(批准号:IGCEA-1107)
  • 【文献出处】 震灾防御技术 ,Technology for Earthquake Disaster Prevention , 编辑部邮箱 ,2014年04期
  • 【分类号】P315.2
  • 【网络出版时间】2015-11-10 09:54:58
  • 【下载频次】93
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