观音峡 meaning in Chinese
guanyin xia
Examples
- Water invasion bursten out during the railway - tunnel construction is usually the mainly problem in constructing or operating , also which brings surface water to exhaustion and pollutes environment or effects ecology , etc . the geleshan tunnel which crosses through guan - yin gorge anticline which trend is near south north , is located between tuanjie village and jingkou village of the shapingba zone , chongqing city , which is belongs to the inducting segment of yu - huai railway . the guan - yin gorge anticline appears to ridge and slot interlacing in land form , and is composed of clastic rock and carbonate rock from jurassic xintiangou group to triassic
歌乐山隧道位于渝怀线引入段重庆市沙坪坝区团结村至井口村之间，隧道穿越近南北向的观音峡背斜，地貌上表现为脊、槽相间，观音峡背斜由侏罗系新田沟组至三叠系下统碎屑岩和碳酸盐岩组成，歌乐山顶大部分出露可溶岩地层，地表岩溶发育，有大量泉水和暗河出口，并修建有多个中小型水库、大量池塘和水井。 - First , on the base of investigating geleshan geologic environments , the author carefully analyzes them , studies their water storage structure , discusses the relationship of underground water dynamic changes and tunnel drainage by desiccation ; secondly , the author makes the dynamic analysis , regression analysis , routine hydrochemistry analysis , isotope analysis , so draws to guan - yin gorge anticlire east and west slot ' s karst developing features , alternated conditions underground water and supplying drain ways ; thirdly , by stating the fissuring ' s surveying data , the author calculates the seeping tensor
作者在进行歌乐山地质环境调查的基础上，仔细分析了大量观测资料，研究其储水构造，掌握地下水动态变化与隧道施工涌水的关系，及补给受降雨的影响情况。对隧道周围的地下水进行动态分析、回归分析、常规水化学分析以及同位素分析，得出观音峡背斜东西翼槽谷的岩溶发育特征，及地下水的循环交替条件、补给排泄途径；统计分析裂隙测量数据，计算渗透张量。