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1)  Shizong-Mile fault belt
师宗-弥勒断裂带
2)  Shizong-Mile zone
师宗-弥勒带
1.
The study areas are located in the Jinshajiang zone,NW Yunnan and SW part of the Shizong-Mile zone (Jianshui),SE Yunnan respectively,and tectonically belong to the east part of the Paleo-tethys tectonic domain.
研究区分别位于滇西北金沙江带和滇东南师宗-弥勒带西南段建水地区,构造上位于古特提斯构造域的东段,其中滇西北金沙江带是扬子陆块与冈瓦纳陆块的交汇部位,而师宗-弥勒带则分隔了扬子陆块与华夏陆块。
3)  Yale Xiongle fracture belt
亚勒-雄勒断裂带
4)  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。
5)  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。
6)  Kuerle fault
库尔勒断裂
1.
Among these faults, Kuerle fault, which cuts through northern part of Kuerle, has new and strong activity.
尤其斜切库尔勒市区北部的库尔勒断裂,新活动十分强烈。
补充资料:弥勒问本愿经
【弥勒问本愿经】
 (经名)弥勒菩萨所问本愿经之略名。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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