山带基本解释

汉语拼音:shān dài

指环绕峰岩的带状白云。

山带详细解释

  1. 指环绕峰岩的带状白云。

    唐 韩翃 《送客归江州》诗:“风吹山带遥知雨,露溼荷裳已报秋。” 宋 陈舜俞 《庐山记》卷一:“ 张野 《庐山记》:‘天将雨,则有白云冠峰,或亘巖中,俗谓之山带,不出三日,必雨。’”

山带双语翻译,山带在线翻译例句

    • Garze - Litang fracture zone separates Yidun orogenic belt from Yajiang folded belt.

      甘孜 - 理塘断裂带是义敦造山带与雅江褶皱带的分界断裂.

    • South Tianshan: a Late Paleozoic or a Triassic orogen?

      南天山: 晚古生代还是三叠纪碰撞造山带?

    • Monte Cristo looked upon Morrel with indescribable tenderness.

      基督山带着无法形容的怜爱望着莫雷尔.

    • The eastern Tianshan porphyry copper belt is located on the southern margin of Tuha basin.

      吐哈盆地南缘斑岩铜矿带位于中亚造山带东天山的中段.

    • 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.

    • Dabie mountains are a collision orogen between the Yangtze and the North China blocks.

      大别山为扬子陆块和华北陆块之间的碰撞造山带.

    • 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.

    • The Danba area is located in the central part of the Songpan - Ganzi orogenic belt.

      丹巴地区位于松潘—甘孜造山带中部.

    • Clenched in the volcanic fist, the huge Basin was created By the motion of crustal plates.

      这个巨大的盆地坐落在火山带内, 它是由地壳板块的运动所造成的.

    • Beihuaiyang basin and range structural belt is an important part of Dabie orogenic belt.

      北淮阳盆岭构造带是大别造山带的重要组成部分.

    • Nam breasted mountain with the sea, beautiful scenery, monuments are spread all over.

      南安襟山带海, 风光秀丽, 名胜古迹星罗棋布.

    • The Baguamiao gold deposit is the only super large gold deposit in the Qinling orogen.

      八卦庙金矿是秦岭造山带唯一的超大型金矿床,曾被认为是微细浸染型(卡林型)金矿.

    • Altai orogeny , as one of notable crustal accretion areas, is famous for its abundant mineral deposits.

      阿尔泰造山带是中亚地区显生宙大陆地壳增生明显的地区之一, 蕴藏丰富的矿产资源.

    • The Qiushuwan copper deposit Qinling Group lies in the south of the North Qinling orogenic belt.

      秋树湾角砾岩型铜(钼)矿位于北秦岭造山带南侧,含矿地层为秦岭群.

    • The South Tianshan range formed end of the Carboniferous orogen was formed under the strong compression.

      自石炭纪末,南天山全面遭受挤压抬升形成复杂的造山带,二迭纪开始南天山进入大陆演化阶段.