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- The Moho upheaves at the basin center and dips toward the basin edge. 莫霍面形态中部上隆，盆地南北边缘分别向南、北加深；
- Even further south, reflections from 35km 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.
- Any of several flightless New Zealand birds,now rare,of the genus Notornis,especially the takahe. 短翅水鸡一种新西兰的现为稀有动物，短翅水鸡属，尤指黑水鸡
- Any of several flightless New Zealand birds, now rare, of the genus Notornis, especially the takahe. 短翅水鸡一种新西兰的现为稀有动物，短翅水鸡属，尤指黑水鸡
- The rise of the asthenosphere,the position of Moho and mantle plume are the indication of the mantle convection. 软流圈上涌高度、莫霍面或地幔羽的位置是地幔对流的具体的表现。
- Moho depth increases from 33 to 34 km on east side and from 36 to 38 km on the west side. 断裂带东侧莫霍面埋深浅;大约为33~34km; 西侧莫霍面埋深明显增加;达到36~38km.
- The Qinling Moho zone formed after crust balance play so-called “the foot of a hill” role. 受地壳均衡作用的影响，已形成的秦岭壳幔过渡带起到了通常所说的“山根”作用。
- There exists a deep fault cutting the Moho or a anomalous deep structure in the epicenter region. 在震区的下方存在著M面断裂或构造异常带。
- There are parallel or cross relationships between geochemical boundaries and gravity, Moho and magnet gradisnts. 地球化学边界的形成与板块的斜结合以及结合以后岩石圈结构调整产生的克拉通边界密切相关。
- The relationship between Moho swell and modern morphological feature appear the mirror plane. 松辽前寒武古陆块 (含开鲁坳陷 ) ,是大中型移置体 ;
- The uplift-depression of the magnetic basement is more orless conformable with that of the Moho in Central and Southern Jiangsu,Western Zhejiang and Southern Anhui. 在苏中、苏南、浙西、皖南地区,莫霍面与磁性基底升降大体一致。
- Based on the inversion result from deep seismic sounding and natural earthquakes, this dissertation gives out the contour map of Moho interface in the research region. 本文利用人工地震测深和天然地震资料反演得到莫霍面深度的数据给出了研究区内莫霍面的等值线图。
- The Bouguer gravity anomaly in Tibetan Plateau is decomposed by wavelet transform and low-pass filter respectively,and applied to the inversion of Moho. 分别采用小波变换和低通滤波对青藏高原地区布格重力异常进行了位场分解和莫霍面反演,并将反演结果与地震资料作比较。
- In this paper,the Moho depth in the region of the Ryukyu trench arc basin system was calculated using the technology of a 3 D generalized inversion. 本文利用三维广义反演技术对重力资料进行反演，计算出了琉球沟弧盆系地区的莫氏面深度。
- The inversion results demonstrate that the Moho depths of Qinghai-Tibet plateau are shallow around the edges, and deep at the center. 结果表明，青藏高原莫霍面呈现出边缘浅、中部深，边缘变化快、梯度大，中间变化梯度趋缓的特点。
- 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。
- The inversion results demonstrate that the Moho depths of Qinghai-Tibet plateau are shallow around the edges,and deep at the center. 结果表明,青藏高原莫霍面呈现出边缘浅、中部深,边缘变化快、梯度大,中间变化梯度趋缓的特点。
- The velocity structure features of sediment, basement, upper crust, lower crust, Conrad and Moho interfaces were analyzed. 分析了沉积层、基底、上地壳、康腊面、下地壳和莫霍面的特征。
- The figures of Bouguer anomalies and vertical magnetic anomalies obtained at the scales of 1:1000 000, 1:500 000 and 1:100 000 were processed and the Moho depths were calculated. 本文对天山南麓1:100万、1:50万和1:10万布格重力异常图及相应的垂直磁力异常图进行了处理,并计算了莫霍面深度。
- In this paper, PS reflection was used to determine the depth and fluctuation of Moho discontinuity in the local region of the north side of the Yarlung Zangbo River. 本文利用PS反射波探测了雅鲁藏布江北侧局部地区莫霍面的深度和起伏。
