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山间盆地的英文

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"山间盆地"怎么读用"山间盆地"造句

英文翻译手机手机版

  • hollow
  • intermont basin
  • intermontance basin
  • intermontancebasin
  • intermontane basin
  • intermount basin
  • intermountain basin
  • intermountbasin
  • orographic basin

例句与用法

  • Intermontane basins in relatively stable regions subjected to regional uplift .
    较稳定区域内的山间盆地,曾有过区域隆起。
  • Intermontane interamontane intermont basin
    山间盆地
  • Santanghu basin is a congruent & reconstruct innertief , which developed on the basis of rift - fault basin of permian
    三塘湖盆地是一个在二叠纪裂谷-断陷盆地基础上发展起来的叠合、改造型山间盆地
  • And the yalong river . near sthe water - dividing ridge , appear quite a few mountain basins used by the lacals as grazing area . glacier lakes are widespread in the hundreds in the area between litang and daocheng county alone
    在分水山脊出现不少山间盆地,冰川湖四处可见,仅理塘至稻城间旧有数以百计。
  • This basin had undergone three phases , the rifting phase in permian , the depression phase from mesozoic to early neozoic and the phase which formed the intermountain basin by thrusting reformation latter neozoic
    盆地演化经历了二叠纪裂谷盆地、中生界至新生界代早期的陆内坳陷盆地和新生代晚期的逆冲改造山间盆地三个阶段。
  • Being primarily controlled by northwest faults , cretaceous of jiyang depression contained several isolated basins , and lake levels of these isolated basins were instable , but on the whole , shore and shallow lake sub - facies is in the majority
    北西向断层的活动对沉积起到主要的控制作用,在其控制下,白垩纪济阳坳陷为一相互分割的山间盆地,湖盆范围时大时小,湖水深度不断变化,总体湖水较浅,主要发育滨浅湖亚相。
  • Yanqi basin is an intermont basin of tian shan , there is a nww trending right lateral strike slip active fault in southwestern basin , its maximum slip distance is 210m , and slip rate is about 10mm / yr , moreover , there is a west - east trending active anticline along northern basin
    焉耆盆地是一个天山山间盆地,盆地西南缘发育一条走向北西西的右行走滑活动断层,最大走滑距离为210m ,走滑速率约10mm / yr ,盆地西北缘发育走向近东西的活动褶皱。
  • Tian shan extends east - west in central asia , the tian shan range was formed in later paleozoic , and a few intramontan basins appeared in mesozoic . it uplifetd again in early miocene because of the north - south compression induced by the india - asia collision , so many active structures can be found in tian shan . active tectonics took actions during last ten thousands yeas , and surface traces of fault scarps , detached gullies and folds in alluvial deposit are apparent , so it is easy to distinguish them from other geological phenomema
    天山位于亚洲中部,天山造山带形成于晚古生代,到中生代时,在天山内部形成了一些山间盆地,印度板块在始新世向北与欧亚板块碰撞,天山受南北向挤压力的作用再度于早中新世隆起,由于板块碰撞的持续进行,在天山山间及山前发育了许多的活动构造。
  • The basement of the basin is consist of precambrian crystal basement and paleozoic folding basement , while the cover has undergone the evolution of intra - continental rife in permian , down warped basin in triassic - cretaceous period and inter - mountains basin in tertiary . the main sediments are huge - thick volcanic rock , shallow intrusive rock and tuff in early permian , dark mudstone , marl and muddy dolostone in lucaogou formation in middle permian , huge thick volcanic rock , intruder in tiaohu formation in middle permian , miscellaneous sandy gravel , sandstone and gray mudstone in triassic ( the red is under the gray , and huge - thick dark gray , gray sandy gravel , sandstone , mudstone with coal layer in jurassic
    盆地基底由前寒武纪结晶基底和古生代褶皱基底组成,盆地盖层则经历了二叠纪的裂谷盆地、三叠纪?白垩纪的坳陷盆地和第三纪后的山间盆地的演化过程。盆地主要沉积了下二叠统巨厚火山岩、浅成侵入岩和凝灰岩;中二叠统芦草沟组的暗色泥岩、泥灰岩、白云质岩石以及条湖组的巨厚层火山岩、侵入岩;三叠系杂色砂砾岩、砂岩及灰色泥岩(下红上灰) ;以及侏罗纪厚层深灰、灰色砂砾岩、砂岩、泥岩夹煤层。
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