1) fracture zone water
断裂带水
2) water conducted zone
导水断裂带
1.
Analysis the height of water conducted zone of coal seam roof based on GA-SVR
基于遗传-支持向量机法的煤层顶板导水断裂带高度的分析
2.
With the nonlinear finite element numerical simulation method,the height of water conducted zone near fault was simulated in fully mechanized top-coal caving face considering two different faults obliquities(75° and 35°) and the relation between the mining direction and fault obliquity.
采用非线性有限元数值模拟方法,考虑不同断层倾角大小(75°和35°)、工作面推进方向与断层倾向关系,模拟了在断层影响下厚煤层综放开采引起的导水断裂带高度,得出了综放开采2种倾角断层、不同推进方向4种组合的导水断裂带高度随煤层开采动态发育规律示意图。
3) Hengshui fault zone
衡水断裂带
1.
In Jizhong depression, Hengshui fault zone is of characteristics of transfer zones, which divided the depression into two north and south regions.
冀中坳陷衡水断裂带具有构造调节转换带性质 ,它明显地将坳陷分为南北两区。
4) water rich fractured band
富水断裂带
5) Zhoucheng-Qingshui fault zone
周城-清水断裂带
6) Xianshuihe fault
鲜水河断裂带
1.
Earthquake simulation of Xianshuihe faults;
鲜水河断裂带的地震模拟
2.
Deformation accumulative rates of Xianshuihe faults and prediction effect assessing;
鲜水河断裂带形变累积率及其效能评价
3.
In this paper,we calculate the torsion,tension and vertical deformation of the Xianshuihe fault over the years and discuss the fault activity behavior on the basis of deformation of the measuring point along the fault based on the observational data of short leveling and baseline along the Xianshuihe fault since 1981.
利用1981年以来鲜水河断裂带跨断层短水准、短基线观测资料,计算多年来断层的水平扭错、水平张压以及垂直升降变化量,以此分析各测点断层随时间推移的活动习性。
补充资料：断裂带
亦称“断层带”。有主断层面及其两侧破碎岩块以及若干次级断层或破裂面组成的地带。在靠近主断层面附近发育有构造岩，以主断层面附近为轴线向两侧扩散，一般依次出现断层泥或糜棱岩、断层角砾岩、碎裂岩等，再向外即过渡为断层带以外的完整岩石。断层带的宽度以及带内岩石的破碎程度，决定于断层的规模、活动历史、活动方式和力学性质，从几米至几百米甚至上千米不等。一般压性活压扭性断层带比单纯剪切性质的断层带宽。在一些大型的断层带中，由于被后期不同方向的断层切错，和夹有一些未破碎的大型岩块，只是断层带的结构趋于复杂化，从而在近代的断层活动中容易形成运动的阻抗，是应力易于积累和发生地震的场所。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条