鲜水河

基于GPS技术的活动断裂监测&以鲜水河、龙门山断裂为例

Monitoring of Faults Activity Based on GPS

鲜水河断裂带热水水文地球化学特征及形成模式

The hydrogeochemical characteristics and forming model of hot water in the Xian shui-he fracture zone

各类构造应变场的最高值都出现在喜马拉雅构造带与昆仑山地块内（地震断裂带南侧），鲜水河安宁河断裂带次之。

The maximum of strain rate exists in the Himalaya tectonic zone and Kunlun mountain block .

并初步将该方法应用于鲜水河断裂带的地震趋势分析。

Its application is preliminarily to the tendency of earthquake occurrence of the Xianshuihe fault in this paper .

活动断裂带中遥感数字图像处理技术&以鲜水河活动断裂带为例

The technique of TM data image processing in the investigation of active fault zone ── xianshuihe active fault zone as an example

同时，鲜水河断裂带之乾宁-康定一带已形成闭锁区。

Simultaneously , it is pointed out that the blocking zone is made up in the Qiannin & Kangdin area of Xianshuihe fault zone .

而岩性差异对东昆仑断裂和金沙江&鲜水河断裂的断层两盘的红外亮温影响较大；

Rock differences have major influence on the IR brightness temperatures on the both sides of the eastern Kunlun fault and the Jinshajiang-Xianshuihe fault .

而昆仑山地块中部、鲜水河断裂带和云南中部地区，其应变速率最大，速度变化最快；

Large strain rates are found in the areas as Kunlun block , Xianshuihe fault zone and central Yunnan , and the variation of velocity is very rapid .

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 .

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 .

在地震时断层水平位错分布研究的基础上，结合地震破裂在断裂带内的分布认为沿鲜水河断裂在乾宁南北两侧存在两个长度不大的地震破裂空区。

Based on a study of the horizontal displacement distribution during earthquakes and combined with the co - seismic fractures layout along the fault belt , two different length gaps without seismic fractures have been suggested at north and south sides of Qianning .