mantle convection

基本解釋

• 地函對流，[地物] 地幔對流；[地物] 地幔對流

英漢例句

雙語例句

• In mantle convection models, the mantle viscosity is generally assumed constant or dependent on depth.
  粘度爲(wèi)常數(shù)或僅隨深度變化是地幔對流模型中常用的假設(shè)。
• The ratio of poloidal to toroidal component of mantle convection determined the proportion of seismic energy released in the thrust, normal, or strike-slip earthquakes.
  地幔對流的垂直運(yùn)動與水平運(yùn)動分量的比率，決定了逆沖、引張與走滑型強(qiáng)震的能量釋放份額。
• A constant viscosity mantle convection model is developed into a variable viscosity model assumed a latitude-dependent viscosity with small fluctuations on the basis of a constant background value.
  建立了一維粘度擾動下的變粘度模型。 通過假定粘度爲(wèi)常粘度背景下存在僅隨緯度變化的小橫曏擾動，將常粘度模型發(fā)展?fàn)?wèi)變粘度地幔對流模型。

• mantle convection更多例句

詞組短語

短語

• Mantle wedge convection 地幔楔對流
• whole mantle wide convection 全地幔對流
• mantle convection circle 地幔對流環(huán)
• mantle convection theory 地套對流說
• mantle 's convection 地幔對流

• mantle convection更多詞組

專業(yè)釋義

地球科學(xué)

• 地幔對流

  In another hand, mantle convection process may directly influence the surface deformation movement of the region.
  另一方麪，地幔對流對巖石層底部的拖曳作用將直接影響該區(qū)域巖石層形變運(yùn)動。

• 地函對流