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The results show that the bedrock moves 8 m en masse when the epicenter is located near the railway,while the Quaternary loose sediments and groundsill are deformed.The horizontal diaplacement of the Quaternary close to the fault is obviously smaller from above downward,while the rails and groundsill show successive left-lateral crooked deformation for about 25 m.There occur a NE-trending tensional graben and a NW-trending seismic drumlin on the east and west sides of the railway respectively.

结果表明,震中位于铁路线附近时,基岩整体移动,而第四纪松散层和道床则发生了变形,靠近断裂带附近的第四系自下而上水平位移明显减小,而铁轨和道床没有明显的断错,表现为长度约为25m的连续左旋弯曲变形;在铁路东、西两侧形成NE向的张裂陷和NW向的地震鼓包。

In Late Jurassic period (159-135Ma), when the orientation of maximum principal compressive stress was NW direction, the Wuzhangshan granite intruded to upward, accompanied the formation of NW trending Sanrenchang and Huangshuian breccia pipe belts; In the Early Cretaceous period (135-120Ma), when the orientation of maximum principal compressive stress was NNW trending, the second stage of Huashan granite intruded to upward, accompanied the formation of NW trending Qiyugou breccia pipe belts; In 120-105 Ma, when the orientation of maximum principal compressive stress changed to NE direction, the gold-bearing quartz veins and gold orebodies in breccia pipes were formed along the NE trending fractures; In the Middle Cretaceous period (105-85 Ma), when the orientation of maximum principal compressive stress was NEE, the NEE trending Leimengou granite porphyry intruded to upward, accompanied the formation of NEE trending Leimengou breccia pipe belts.

在晚侏罗世(159~135Ma),构造应力场最大压应力方向为NW向,形成了NW走向的五丈山岩体以及NW向展布三人场、黄水庵两个角砾岩带;在白垩纪早期(135~120Ma),最大压应力为NNW向,形成了花山岩体第二期上侵,并伴有NW向的祁雨沟角砾岩带;其后(120~100Ma),构造应力场最大压应力方向变为NE向,形成了NE向含金石英脉及角砾岩体中金矿体;最后(100~80Ma),形成了雷门沟花岗斑岩以及NEE向展布的雷门沟-杨河沟角砾岩带(区域构造应力场的最大主压应力方向为NEE向)。

The Geopark is situated at the junction of the north east trending Yanshan tectonic belt and the north-north east trending Taihanshan tectonic belt ,and is one of the typical intracontinental orogenic belts in China having complicated geological background.

园区地处北东向燕山构造带和北北东向太行山构造带衔接区内,是我国陆内造山带的典型地区之一,具有复杂的地质背景。

In the study, the authors considered the formation mechanism of the "y"- type structure as follows : the EW - trending compression stress field was derived from the sinistral strike - slip of Wufengxian - Tiesitang fault in Indosinian orogeny and the traction of the sinistral strike - slip made the NNE -trending structural lineament produce sinistral torsion in the west part of the Anren county seat, thus the NNW - trending folds were resulted.

研究认为,"y"字型构造形成机制为:五峰仙-铁丝塘断裂在印支运动中具基底左旋走滑性质,走滑所派生的近东西向挤压应力场,及走滑所产生的牵引作用,使安仁以西NNE向构造线产生逆时针旋转,从而形成NNW向褶皱。

The Neogene fractures widely developed in the study area may be classed into two groups: NW-trending and NE-trending.

神狐海域断层发育,可分为晚中新世活动的NW向断层和上新世以来活动的NE断层两组。

A study of regional geological setting and ore-control factors for the Xiasai Ag-Pb-Zn deposit indicates that NW-trending structures act as conduits for ore fluids and orebodies are controlled by a NNw-trending fault system, while ore shoot s are confined equidistantly to secondary structures associated with the NNW-trending fault system.

研究结果表明,富矿体在NNW向断裂中按一定间距连续出现,并在NNW向断裂伴生的次级构造中集中产出。

337 Uranium ore deposit lies to the east of the Xiazhuang orefield,and there are structural fracture groups with EW,NNE-trending,diabase and syenite vein with NW-trending in the deposit region.

337铀矿床位于下庄矿田东缘,区内发育近EW向、NNE向构造裂隙群及NW向辉绿岩和正长岩脉体,发育以碱性为主的多种围岩蚀变。

The Huade Group underwent at least two phases of deformation:the early phase of deformation gave rise to ENE-trending synclinorium and the late phase was marked by tectonic superimposition,forming NNW-trending folds. The main phase of deformation likely occurred in ~2.0 Ga B.P.The deformation of the Huade Group is related to a Paleoproterozoic orogenic event along the northern margin of the North China Craton, which has great significance for the study of accretion and breakup of the North China Craton.

化德群经历了两期构造变形,早期为北东东走向的复式向斜,晚期又遭受了构造叠加,形成了北北西向褶皱构造,其主期变形可能发生在2.0 Ga左右,它的褶皱造山是华北克拉通在古元古代向北增生的体现,这对研究华北克拉通的增生,裂解具有重要意义。

The karst landform tailings dam disaster appraisal and the safe monitor are important for reducing the risk and the accident. The most prominent factors of influencing the stability of Karst landform in some tailing dams are NW-Trending and NE-Trending Structure's "tabular pattern", bad rock mass globality, highly-jointed, karst, miarolitic, the earth's surface -underground "ladders" fluent movement pattern; the effect of the flood and the earthquake.

摘 要:影响岩溶地貌某尾矿坝坝体稳定问题最突出的因素是:北西向、北东向构造的&棋盘格式&;岩体整体性差、节理化;岩溶、洞隙、地表―地下&阶梯&水流运动模式;洪水和地震影响。

Because the area on the east part of the Anren county seat is near the regional primary subduction - fault, namely the NNE - trending Chaling - Chenzhou fault, the Wufengxian - Tiesitang NW- trending fault had little strike -slip measure, so the derivative stress and traction were smaller, and at the same time the regional NWW- trending principal stress was stronger, which produced NNW -trending folds.

安仁以东由于紧邻NNE向茶陵一郴州主俯冲汇聚断裂,NW向断裂走滑量相对较小,派生应力与牵引效应小,而区域NWW向挤压应力大,从而于断裂两侧均形成与区域构造线一致的NNE向褶皱。

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