峡谷区的英文

• canyon country

• "峡谷"英文翻译    gorge; canyon; water gap; gu ...
• "区"英文翻译    H region; H
• "峡谷区国家公园" 英文翻译 :    canyonlands national park
• "河谷区" 英文翻译 :    cotes du rhone; riverdale
• "平谷区" 英文翻译 :    pinggu district
• "涩谷区" 英文翻译 :    shibuya, tokyo
• "田谷区" 英文翻译 :    setagaya
• "峡谷" 英文翻译 :    gorge; canyon; water gap; gulch; trench; glack; slap; chasm; kloop; [法国] couloir; pongo; poort; clough, claugh; clech, cleugh; barranca,barranco; [南非] donga; glen; quebrada (美国西南部); [阿拉伯] kheneg; [印度] khud; [北非] khor; combe, coombe, coom, coomb; [英方]goyle; flume 大峡谷国家公园 [美国] grand canyon; 悬崖峭壁之间的峡谷 a gorge between precipices; 那条大路穿过峡谷。 the main road goes through the mountain gap
• "保土谷区" 英文翻译 :    hodogaya-ku, yokohama; hodogayachō; kasumidai
• "世田谷区" 英文翻译 :    setagaya, tokyo; setagaya-ku
• "曼谷区名列表" 英文翻译 :    list of districts in bangkok
• "冰峡谷" 英文翻译 :    donga
• "侧峡谷" 英文翻译 :    side canyon
• "大峡谷" 英文翻译 :    dsd (tide in grand canyon); grand ganyon; the grand canyon; the great canyon; the great valley; the missouri breaks
• "沟峡谷" 英文翻译 :    ravine
• "海峡、峡谷" 英文翻译 :    pertuis
• "梦峡谷" 英文翻译 :    dream canyon
• "山口、峡谷" 英文翻译 :    collado
• "深谷，峡谷" 英文翻译 :    gulch
• "深峡谷" 英文翻译 :    barrage; barranco; couloirs
• "吞咽，峡谷" 英文翻译 :    qorge
• "雾峡谷" 英文翻译 :    firemyst gully
• "峡；峡谷" 英文翻译 :    gorge
• "峡谷、山涧" 英文翻译 :    schlucht
• "峡谷坝" 英文翻译 :    gorge dam; valley dam

• At the same time watertight rock surround the carbonate rock , which is helpful to water percolate deeply and trigger earthquake
  同时，峡谷区碳酸盐类岩石周围又有弱透水和微透水的岩层包围着，有利于库水向深部渗透，诱发地震。
• The 6 regions , including the contiguo us areas of southwest sichuan and northwest yunnan , the west part of sichuan , th e contiguous areas of sichuan , guizhou , hubei and hunan etc . , should be conside red as the key ones for conservation in the yangtze basin
  川西南滇西北、川西高山峡谷区、川鄂湘黔接壤区、南岭山地北部6个区域成为长江流域自然保护的关键区域。
• Based on geochemical technical tests conducted in the yanzidong ore block , western yunnan , the authors used the hydrochemical survey as the grade 3 inspection method for high canyon target areas , and rearranged the methods for routine stream sediment survey and soil survey
  摘要根据在滇西燕子洞矿段的化探方法技术试验研究结果，将水化学测量作为高山峡谷区靶区三级查证的方法，并对常规水系沉积物测量、土壤测量的工作方法进行了调整。
• Although the empirical formula ? = yh [ 14 . 7 ( rwrlogd ) + 3 ] has been applied successfully to some engineerings , but it is a general formula , not one specially for rocky bank slope in gorge area . so the author constructs a statistical formula smr
  71n (只log0 ) + 13 ]在工程实践中的应用效果较好，但该公式是建立在大量统计资料上的通用公式，并不专门针对峡谷区桥基岸坡，因此作者基于smr方法，统计拟合出适用于峡谷区桥基岸坡的经验公式?夕： 2
• Depending on how the ground surface is denuded , the feature of the current crustal stress field and rock stress environment can be calculated analyzing the result in this paper : by analyzing the recovering feature of the elastic deformation of the rockmass in unload - stage under various pressures , it has been found there is close relationship between the recovering degree of the elastic deformation of the rockmass and the unloading degree of the pressure the direction of the major principal stress in the crustal stress field is not consistent with the direction of the crushing stress regional tectonics borne during the last tectonic movement . the evolving degree of the regional geomorphology evidently affects the current crustal stress field , which changes from the self - weight stress field to the horizontal stress field , with the changing of the eroding degree of the regional geomorphology ranging from valley area to hilly country to flat country . in valley area , where there is two stress belts , the bankslope s tress belt and the self - weight stress belt within the mountain . the direction of the major principal stress is nearly parallel to the ground surface and inclines towards the valley in the bankslope stress belt . it is nearly vertical in the self - weight stress belt
  通过本文的研究成果，根据区域性地貌的演化特征，我们可以大致地对现今地应力场进行判断：在分级卸荷条件下，岩体中弹性变形的恢复具有明显的规律性，这种规律对于研究地应力场的演变是有帮助的；地应力场中最大主应力方向与区域构造形迹在最近的构造运动中所受区域性挤压应力的方向无明显的对应性；区域性地貌形态的演化程度对现今地应力场的特征具明显的影响，随着区域性地貌侵蚀程度由峡谷区、丘陵区、平原区的变化，现今地应力场特征由自重应力场、水平应力场为主含少量自重应力场特征向水平应力场的规律变化；在峡谷区，山体中具有两个应力带：自重应力带和卸荷应力带，最大主应力方向在卸荷应力带中近平行于坡面并倾向于河谷、在自重应力带中近于直立；根据原始地面遭剥蚀的程度，可以大致地估算最大主应力和中间主应力的量值和方向；在丘陵区和平原区，最大主应力的方向近于水平，并与附近区域性侵蚀盆地和河流的展布方向基本平行，根据原始地面遭剥蚀的程度，可以大致估算其最大主应力的量值；根据区域性地貌形态的特征来分析工程区的现今地应力场特征，并进而大致了解岩石的应力环境，这种分析方法得出的结论与许多实际的地应力测试成果基本一致，对于大型水电工程地下厂房和压力隧洞的设计是有所帮助的。
• This thesis puts forward a systemic method to analyze stability of bridge bank slope in gorge area . it includes elementary field geological evaluation , calculation of stable angle of bank slope with empirical formula , simulation of slope stress state with fem and rockmass strength judgement . then rational laying position of bridge piers can be confirmed
  本文提出了峡谷区桥基岸坡的稳定性分析的系统方法，包括野外初步地质评价、经验公式法确定岸坡稳定坡角、岸坡应力场的有限元模拟及强度分析，进而综合评价岸坡稳定性，并确定桥基合理埋置位置。
• Relating closely to the main problem of the high sidewall and wide span underground cavities excavation stability of xiluodu hydroelectric project , the evolution characters of geo - stress field in deep - cutting gorge and the whole features of the stress field , strain field and plastic failure zone around the underground chambers after excavation are studied systematically in the dissertation , based on a great deal of data gathered in field investigation and taking the flac3d v2 . 0 software as basic computation tools . meanwhile , in the course of research , the new methods of dynamic numerical simulation are summarized and applied . furthermore , the effects of rock mass qualities , initial geo - stress field and excavation procedure on surrounding rock mass stability are discussed
  本文紧密结合溪洛渡水电工程大跨度、高边墙复杂地下厂房洞室群，施工开挖过程中和开挖后围岩稳定性研究这一重大课题，在详尽的野外地质调查工作和对大量基础地质资料的整理与分析基础上，以目前国际工程地质界公认的最新通用软件flac ~ ( 3d ) 2 . 0版作为基本计算工具，从整个坝区地应力场的研究开始，通过动态数值仿真分析这一新的模拟思路，系统地研究了深切峡谷区地应力场多阶段的特征和演变规律，进而对左、右岸地下厂房洞室群开挖全过程中围岩应力场、变形场和塑性破坏区的变化特征，进行了全过程动态数值仿真研究，并详细讨论了围岩质量、初始地应力场、施工开挖顺序对大型地下洞室群围岩稳定性的影响。
• ( 3 ) according to the new methods of dynamic numerical simulation analysis , the computation model of the deep cutting gorge is contracted with flag30 software and flag30 pre - processing package , the reasonable simulation course is designed and the calculating results is controlled effectively . finally , the forming process and the evolution features of the 4 stages geo - stress field evolution in xiluodu gorge are displayed in the paper , from which the variable regulations are analyzed and summarized systematically . these achievements can be regarded as creditable evidences for technocrats to solve some problems of geo - stress field in xiluodu area
  ( 3 )按照动态数值仿真新思路，运用flac ~ ( 3d )软件及flac ~ ( 3d ) pre - processingpackage ，建立了深切峡谷区仿真计算模拟，设计出了较为合理的仿真过程方案，有效地控制了结果的输出，重现了峡谷形成过程中四个发育期的地应力场特征，并对峡谷区地应力场的演变过程进行了动态的系统研究与分析，其研究成果对分析、解决溪洛渡深切峡谷区地应力场存在的难题，提供了可靠且有力的依据。
• The evolving degree of the regional geomorphology evidently affects on the features of the current crustal stress field . so the crustal stress fields change from the self - weight stress field to the horizontal stress field with the changing of the eroding degree of the regional geomorphology from valley area to hilly country to flat country
  然而，区域性地貌的演化特征对现今地应力场具明显的控制性，当区域性地貌特征从高山峡谷区向低山丘陵区和平原残丘区转变时，现今地应力场的特征也从自重应力场向水平应力场转变。