小江断裂带
小江断裂带
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对小江断裂带的断层泥进行了实验研究。
An experimental study on the gouge along Xiaojiang fault has been carried out .
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而在滇中地区&小江断裂带却是另一番景象,该区样品中的幔源氦平均约占总氦的2.27%,最高也才8.9%。
The mantle-derived Helium of all samples averagely occupies the whole Helium about only 2.27 % , the maximum about 8.9 % .
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本文通过小江断裂带的地震活动规律,认为断裂在具有特征地震复发行为的同时,在特征地震之间还有次级破坏性地震。
By analyzing the seismicity of the Xiaojing fault , the authors believe that there are also secondary-destructive earthquakes between the characteristic earthquakes in the fault .
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鲜水河断裂带、小江断裂带、龙门山断裂带每年垂向变化速率值小,而安宁河&则木河断裂带变化幅度相对较大;
The vertical change rates are small along Xianshuihe , Xiaojiang and Longmenshan fault belts , but the vertical change rates along Anninghe and Zemuhe fault belts are comparatively large .