Moho

基本解釋

• [moho ]地殼與地幔間的界限

同根派生

• Moho相關詞

英漢例句

• The Moho upheaves at the basin center and dips toward the basin edge.
  莫霍面形態(tài)中部上隆，盆地南北邊緣分別向南、北加深；
• Even further south, reflections from 35km depth may correspond to the Moho of peninsular India.
  再往南從35公里深度來的反射波是來自印度半島的莫霍界面.
• The rise of the asthenosphere,the position of Moho and mantle plume are the indication of the mantle convection.
  軟流圈上涌高度、莫霍面或地幔羽的位置是地幔對流的具體的表現(xiàn)。
• Moho depth increases from 33 to 34 km on east side and from 36 to 38 km on the west side.
  斷裂帶東側(cè)莫霍面埋深淺;大約為33~34km; 西側(cè)莫霍面埋深明顯增加;達到36~38km.
• The Qinling Moho zone formed after crust balance play so-called “the foot of a hill” role.
  受地殼均衡作用的影響，已形成的秦嶺殼幔過渡帶起到了通常所說的“山根”作用。

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