1) the eastern Kunlun active fault zone
东昆仑活动断裂带
1.
By Studying on the eastern Kunlun active fault zone based on information of remote sensing image, the recognition models of active fault zone in remote sensing image are built, and we have found its subsidiary active fault zone The eastern Kunlun active fault zone is a natural landscape, geological disaster and climate transfer zone in Qinghai province Those are recognition macromark
基于遥感影像( T M 影像、黑白航片) 信息对东昆仑活动断裂带进行了研究,建立了活动构造影像空间信息识别模式,发现了新的分支活动断裂。
3) Eastern Kunlun Fault zone
东昆仑山断裂带
4) East Kunlun Fault
东昆仑断裂
1.
The East Kunlun Fault zone in Northern Tibetan Plateau is a typical active fault zone,characterized by sinistral strike-slip faults.
对东昆仑断裂带西大滩段进行了断错地貌填图和古地震探槽揭露,共揭露出6次古地震事件,它们的年龄分别为10302±651 aB。
5) Eastern Kunlun Fault
东昆仑断裂
1.
Numeric Simulation on Destructive Effect of Golmud-Lhasa Railway Resulting in Stick-Slip Movement of the Eastern Kunlun Fault;
东昆仑断裂粘滑错动对青藏铁路变形效应的数值模拟
2.
For this event, some researchers have developed an analysis method of brightness temperature difference inside and outside the Eastern Kunlun Fault, and have drawn an important conclusion.
利用NOAA卫星热红外遥感图像对东昆仑断裂带进行解译分析 ,并结合红外亮温的数值化处理 ,对比研究了地震活动比较平静的 1 999年和 2 0 0 1年昆仑山 8 1级地震前后的资料。
6) Kunlun fault zone
昆仑山断裂带
1.
Finite difference numerical simulation of trapped waves in the Kunlun fault zone;
昆仑山断裂带围陷波的有限差分数值模拟解释
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