1) Shule River fault
疏勒河断裂
1.
On the basis of characteristics of remote sensing interpretation in the middle region of Shule River fault zone and its north Beishan area,stability evaluations on the construction of Beishan rock mass have been made by analyzing characteristics of gravity,seismicity,stress state of active fault and seismogenic mechanical condition.
以疏勒河断裂带中段及北山地区遥感图像解译资料为基础 ,通过对该地区重力场深部构造特征、地震活动特征以及活动性构造的应力状态、发震力学条件的分析 ,对北山岩体进行了地质稳定性评价 ,认为疏勒河断裂及其北山岩体是地壳稳定性较好的地区。
2.
Based on remote-sensing geology and very-low frequency anomalies of the central part of the Shule River fault zone, this paper,by means of determining concentration of radon emanation at the surface above the fault zone, has analysed and evaluated the stability of the central part of the Shule River fault zone.
本文以疏勒河断裂带中段遥感地质特征及甚低频电磁异常特征为基础 ,通过测定断裂带上部地表的氡射气浓度 ,对疏勒河断裂带中段的稳定性进行了分析和评价。
2) Shule River fault zone
疏勒河断裂带
1.
The stability of Shule River fault zone is mainly dominated by the neotec-tonic movement pattern and strength of its two sid.
疏勒河断裂带以北的北山地区东部稳定性最好,是今后进一步开展高放废物处置场预选工作的重点地区。
3) Shule River
疏勒河
1.
Sustainable utilization and protection of water resources in Shule River basin;
疏勒河流域水资源可持续利用与保护探讨
2.
Investigation on the Community Structure, Spatial Pattern of Populationand Interspecific Association of Tamarix hispida SalineDesert in the Middle Reaches of Shule River;
疏勒河中游刚毛柽柳盐漠的群落结构、种群空间格局及种间联结性的研究
3.
Analysis on the Exploitation of Water and Land Resources and Its Environmental Effects in the Shule River Watershed;
疏勒河流域水土资源开发及其环境效应分析
4) Shulehe River
疏勒河
1.
The Change Characteristics and the Trend Prediction of Streamflow at the Debouchure of Shulehe River;
疏勒河出山径流量变化特征及趋势分析
5) Bayinguole river active fault
巴音郭勒河活动断裂
6) Shule River Basin
疏勒河流域
1.
Study on water resources development and utilization of Shule River Basin;
疏勒河流域水资源开发利用研究
2.
Hydrochemical characteristics in Shule River basin and environment protection/;
疏勒河流域水化学特征及其保护
3.
Study on the dynamic variation of landscape pattern in the middle and lower reaches of the Shule River Basin;
疏勒河流域中下游景观格局动态变化分析研究
补充资料:疏勒河
疏勒河 中国河西走廊三大内陆河流之一。位于甘肃省西北部。源出青海省祁连山脉西段疏勒南山和托来南山之间的沙果林那穆吉木岭。向西北流,经过音德尔达坂东北坡罗沟转北流入河西走廊。谷地宽15~20千米,海拔3800米左右,河道分散、曲折。河流向北流经托来南山,将山地切割成数百米深的疏勒峡谷,两岸山峰高峻,谷地长65千米,平均宽7千米。经昌马、玉门镇、饮马场后,折向西流,接纳踏实河、党河后,入敦煌市西北的哈拉湖,尾闾为间歇性河道、消没于新疆维吾尔自治区东部边境的盐沼之中 。长550千米,流域面积3.9万平方千米。 |
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