Mohos

基本解釋

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(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。