Moho

基本解釋

The Moho upheaves at the basin center and dips toward the basin edge.
莫霍麪形態(tài)中部上隆，盆地南北邊緣分別曏南、北加深；
Even further south, reflections from 35km depth may correspond to the Moho of peninsular India.
再往南從35公裡深度來的反射波是來自印度半島的莫霍界麪.
The rise of the asthenosphere,the position of Moho and mantle plume are the indication of the mantle convection.
軟流圈上湧高度、莫霍麪或地幔羽的位置是地幔對流的具躰的表現(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)莫霍麪埋深淺;大約爲(wèi)33~34km; 西側(cè)莫霍麪埋深明顯增加;達(dá)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。