一条主要的断层带——鲜水河断层带穿过了该区域。
A major fault line the Xianshuihe fault runs through the area.
对鲜水河断裂带10多年的磁力观测资料进行处理。
The observation data of mobile geo-magnetism along Xianshuihe faults for 10 years are analyzed.
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.
因此，鲜水河断开带的石棉县地带已被锁定为在将来可能会产生强震。
Hence, the Shellomian section of the Xianshuihe fault zone is speculated to be currently locked and have the possibility of producing strong earthquake in the future.
因此，鲜水河断裂带的石棉县地带已经被锁定为在未来可能会产生强震。
Hence, the Shimian section of the Xianshuihe fault zone is speculated to be currently locked and have the possibility of producing strong earthquake in the future.
利用这种滤波方法处理鲜水河地区多幅镶嵌卫星照片，取得了良好效果。
The fine results have been acquired when this filtering method is used to process the multi-sized inlay ERTS photograph of Xianshuihe River zone.
由炉霍、道孚、乾宁三条次级断裂左阶斜列组合而成的鲜水河断裂带的北西段。
The northwest part of Xianshuihe fault consists of three subfractures which are Luhuo, Daofu and Qiannin Faults.
川滇地块东测边界带，由曲江、小江至鲜水河断裂带自南而北现今水平形变量逐渐减小；
Along some eastern boundary belts: Qujiang, Xiaojiang fault belts in the south of Yunnan to Xianshuihe fault belts in northwestern Sichuan, the present horizontal deformation rate decreases.
形变分析结果表明，鲜水河断裂带北段处于蠕动状态，南段则处于应变积累的闭锁状态。
The results of deformation analysis show that the north of Xiansuihe fault zone is in creep and that the south of the fault zone is in locking with strain accumulation.
大的走滑断裂带，如鲜水河断裂，是由主干断裂及与其相伴的若干阶式（或平行）断裂组成。
Some large strike slip faults, such as the Xianshuihe fault, consist of main fault and several sub-faults, which are commonly arranged as en echelon (or parallel) pattern.
部分熔融过程发生于鲜水河断裂早期活动的剪切熔融过程，岩浆作用之前可能发生过强烈挤压而产生了高压变质作用。
The partial melting was probably produced with early shear inching process of Xianshuihe fault belt, also occurred strong compression before the magmatism to produce the high-pressure metamorphism.
本文对鲜水河断裂带南东段，康定断裂地震的形变带进行了分析。认为，地震形变带主要由发育于地形斜坡上的线性坡中槽或垄岗组成。
In this paper, an analysis has been carried out on the Kangding earthquake deformation zone, along the southeast segment of Xianshuihe fault belt.
本文对鲜水河断裂带南东段，康定断裂地震的形变带进行了分析。认为，地震形变带主要由发育于地形斜坡上的线性坡中槽或垄岗组成。
In this paper, an analysis has been carried out on the Kangding earthquake deformation zone, along the southeast segment of Xianshuihe fault belt.
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