1) Lintong-Chang an fault zone
临潼-长安断裂带
1.
The Lintong-Chang an fault zone consists of two main faults and two branch faults.
临潼-长安断裂带主要由两条主断层和两条分支断层组成,断层基本沿北东向的黄土塬陡坎展布,陡坎高30~128m不等。
2.
Our results suggest that these four paleoearthquake events have relation with the activity of Lintong-Chang an fault zone which is then believed to have no strong seismic risk.
根据探槽中地层没有明显错动和临潼-长安断裂带在晚更新世晚期和全新世早期活动较弱,以及历史上无6级以上地震活动记录的特点,本文认为4次古地震事件与临潼-长安断裂带无关,该断裂未来发生强震的危险性不大。
2) Lintong-Chang an fault
临潼-长安断裂
1.
By the observation,measurement and dating to three typical sections at Xiaobaopo,Qiaogou and Zhongdicun,this paper obtained the activity parameters of the Lintong-Chang an Fault since the late Pleistocene and the age stratigraphic sequence of the tablelands of Bailuyuan,Shaolingyuan and Henglingyuan.
通过小鲍陂、桥沟、冢底村3个典型晚更新世断层剖面的仔细观察、测量和年代学工作,获得了白鹿塬、少陵塬、横岭塬3个黄土台塬上临潼-长安断裂晚更新世以来的活动性参数和区域地层的年代序列。
2.
Lintong-Chang an Fault is an important boundary fault between Lishan uplift and Zhouzhi-Huxian depression in Weihe basin.
临潼-长安断裂是渭河盆地内部骊山凸起与周至-户县凹陷之间一条重要的边界性断裂。
3.
The paper is quantitative calculated and analyzed leveling data across fault from 1970 to 1996,leveling data across fault field of Lintong-Chang an fault belt from 1983 to 2004,and gravity data across Lintong-Chang an fault belt from 1992 to 2004.
对临潼-长安断裂带1970~1996年跨断裂水准资料、1983~2004年跨断层场地水准资料和1992~2004年重力段差资料进行了定量计算与分析。
3) Lintong of Xi an
西安临潼
1.
Research on Soil Dryness and the Recovery Below Artificial Forest in Lintong of Xi an;
西安临潼人工林土壤干化与恢复研究
4) Changle-Zhaoan foult zone
长乐-诏安断裂带
1.
It is shown that the deformation characters of Changle-Zhaoan foult zone as a whole are generally the same.
利用福建东南沿海7个跨断层短水准场地20多年的资料,分析了长乐-诏安断裂带的活动特征。
5) Changle-ZhaoanFault Zone
长乐诏安地震断裂带
6) Changdi fault belt
长堤断裂带
1.
Control factors of remaining oil distribution and potential exploitation measures in the northern part of Changdi fault belt;
长堤断裂带北部地区剩余油控制因素与挖潜对策
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