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沉降帶英文

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"沉降帶"怎麼讀用"沉降帶"造句

英文翻譯手機手機版

  • geotectogene
  • su idencezone
  • subsidence zone
  • subsiding belt
  • zone of subsidence
  • zoneofsu idence

例句與用法

  • In the present survey and valuation the area is divided into three parts : exposed karst region in upwarped distric , karst region controlled by folded structures near depressed belts and blinded karst region in fault basins
    目前開展的可有效利用的地下水資源調查評價將該區劃分為隆起帶裸露巖溶分布區、沉降帶邊緣褶皺構造控制巖溶分布區和斷陷盆地隱伏巖溶分布區。
  • During late mesozoic and cenozoic , extensions were widespread in eastern china and adjacent areas . the induced compressions and extensions , uplifting and subsidence as well as large - scale magamatism , increased the pre - existing ne - nne trending faults , uplifts and subsidence belts . this is how ; the giant transform structure led to the formation of xihu depression
    在晚中生代與新生代,拉張作用廣泛分布于中國東部及鄰區,導致了擠壓與拉張、隆起與沉降以及大規模的巖漿作用,于是使早先存在的北東北北東向斷層、隆起帶與沉降帶增強,這也是大的轉換斷層形成西湖凹陷地層的機理。
  • In this case during paleozoic , nearly east west trending arc structures resulted from the interaction between china plate and siberian plate . in mesozoic the westward subduction of kula - pacific plate under the china continental plate resulted in the nne and ne trend structures ( duimadao fault , diaoyudao fault , okinawa fault , uplifts belts and subsidence belts ) as well as volcano - magmatic belts in eastern of china plate
    本文所涉及近東西向展布的弧形構造形成于古生代時期中國板塊與西伯利亞板塊的碰撞帶,而在中生代,中國板塊下的kula - pacific板塊向西俯沖導致了北北東向和北東向構造(如duimadao斷層、 diaoyudao斷層、 okinawa斷層、隆起帶和沉降帶)以及位于中國板塊東部的火山巖漿帶。
用"沉降帶"造句  
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