秦岭基本解释

汉语拼音:qín lǐng

横亘于陕西省中部偏南。东西走向。是黄河和长江两大水系的分水岭,也是中国地理上南北方分界线的一部分。主峰太白山海拔3 767米。

秦岭详细解释

  1. 山名。又名 秦山 、 终南山 ,位于今 陕西省 境内。

    《三秦记》:“ 秦岭 东起 商 雒 ,西尽 汧 陇 ,东西八百里。”《文选·班固<西都赋>》:“睎 秦岭 ,睋北阜。” 李善 注:“ 秦岭 , 南山 也。《汉书》曰:‘ 秦 地有 南山 。’” 唐 韩愈 《左迁至蓝关示侄孙湘》诗:“云横 秦岭 家何在?雪拥 蓝关 马不前。”

  2. 横贯我国中部,东西走向的山脉。西起 甘肃 青海 边境,东到 河南 中部,为我国地理上的南北分界线。

秦岭双语翻译,秦岭在线翻译例句

    • Objective To study the chemical components of volatile oil from Clematis obscura.

      目的研究秦岭铁线莲挥发油化学成分.

    • The new Taibaishan ecology temple is doing just this.

      新近创立的秦岭太白山铁甲生态道观正致力于这方面的工作.

    • ST Qinling, today revealed the progress of bankruptcy reorganization.

      ST秦岭今日披露了破产重整进展.

    • Photinia in south China's provincesand autonomous regions in Qinling.

      石楠产于我国秦岭以南各省区.

    • Protect Qin Ling ecosystem already extremely urgent.

      保护秦岭生态系统已迫在眉睫.

    • The cause of deviation of driving with TBM in Qinling Tunnel is the difficult geological condition.

      由于秦岭隧道部分地段地质方面的原因,使TBM在掘进中发生了偏离现象.

    • The basement in South Qinling, Mianxian Lueyang Yangxian and areasdistributed in some sporadic and is.

      依据陕南秦岭造山带区域地质及重力资料, 按是否露出地表将前寒武纪基底划分为出露基底和隐伏基底两种类型.

    • Taihua complex from the Xiaoqinling area western Henan , consists of supracrustal sequence and granitic gneisses.

      小秦岭地区太华杂岩以多种产状出露于表壳岩系和花岗质片麻岩中,经历了角闪岩相变质作用.

    • Qin - ba mountain area refers to the vast area between Qin - ling mountain range and Da - ba - shan mountain range.

      秦巴山区是指秦岭山脉与大巴山山脉之间的广大区域.

    • The Baguamiao gold deposit in a sort of mesothermal hypothermal carbonate type gold deposit.

      八卦庙金矿床是分布于秦岭造山带中的一种中高温碳酸盐型热液金矿床.

    • In Qinling and Dabashan area, metal resources store of rich with clear mineralization regularity.

      秦岭—大巴山地区金属资源蕴藏丰富,成矿规律明显.

    • The application to constrain strata age is illustrated dating the Cretaceous sediment in western Qinling Mountain.

      本文以西秦岭地区三岔—四店一带的白垩纪地层为例,说明该方法在制约地层年龄中的应用.

    • Quercus aliena var . acuteserrata forest is one of the most important vegetation types of Qinling mountain.

      锐齿栎林是秦岭植被中最重要的类型之一.

    • It changed to ancient land due vertical movement in the end of the Silurian.

      南秦岭在早古生代是扬子板块的被动大陆边缘,在志留纪末曾因垂向隆升变为古陆.

    • The relationship between tectono - magmatic activation and gold mineralization in Qinling, is discussed in this paper.

      本文论述了秦岭区构造岩浆活化作用与金矿床形成及演化的关系.