再往南从35公里深度来的反射波是来自印度半岛的莫霍界面。
Even further south, reflections from 35 km depth may correspond to the Moho of peninsular India.
再往南从35公里深度来的反射波是来自印度半岛的莫霍界面。
Even further south, reflections from 35km depth may correspond to the Moho of peninsular India.
根据艾利的均衡假设,进行了均衡补偿的归算,编制了莫霍界面图和均衡异常图。
According to Airy isostatic hypotheses, a computation of isostatic compensation has been made and a map of M surface and a map of isostatic anomaly drawn up.
在从观测布格重力异常中扣除上述密度异常引起的重力异常后的数据基础上,直接反演了中国西北区域莫霍界面的深度。
Subtracting the gravity anomalies caused by density anomalies from the observed Bouguer anomalies, we inversed the depth of Moho of northwestern China by using the residual anomalies.
根据研究区的重磁资料计算了该区莫霍、居里界面深度与分布。
Using gravitational and magnetic data of the area we calculated Moho and Courier interfaces.
莫霍面是地壳和上地幔的分界面,是个重要的密度界面,东海莫霍面的展布特征,对于研究东海深部构造具有重要意义。
Characteristics of Moho is significant to deep structures in East Sea because Moho is important density inference between Crust and Mantle.
莫霍面是地壳和上地幔的分界面,是个重要的密度界面,东海莫霍面的展布特征,对于研究东海深部构造具有重要意义。
Characteristics of Moho is significant to deep structures in East Sea because Moho is important density inference between Crust and Mantle.
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