鲜水河断裂与龙门山断裂交会区具有特殊的构造性质。
The intersection area of the Xianshuihe fault and Longmenshan fault has a special tectonic nature.
在龙门山断裂带中段的北川地区进行了土壤氡浓度随时间的动态变化定点观测。
The dynamic variation of the Radon-density in soil with the lapse of time has been obtained from surveying at fixed position in Beichuan area along the middle part of the Longmenshan fault zone.
这项研究成果将为评价龙门山断裂带余震和今后强震发展趋势提供关键构造物理参数。
These results provide key appraisal for future assessments of earthquake hazards of the Longmenshan fault zone and aftershock occurrences.
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