您要查找的是不是：
- The Moho upheaves at the basin center and dips toward the basin edge. 莫霍面形態中部上隆，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.
- Any of several flightless New Zealand birds,now rare,of the genus Notornis,especially the takahe. 短翅水雞一種紐西蘭的現為稀有動物，短翅水雞屬，尤指黑水雞
- Any of several flightless New Zealand birds, now rare, of the genus Notornis, especially the takahe. 短翅水雞一種紐西蘭的現為稀有動物，短翅水雞屬，尤指黑水雞
- 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。
- Moho depth increases from 33 to 34 km on east side and from 36 to 38 km on the west side. 斷裂帶東側莫霍面埋深淺;大約為33~34km; 西側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。
- There exists a deep fault cutting the Moho or a anomalous deep structure in the epicenter region. 在震區的下方存在著M面斷裂或構造異常帶。
- There are parallel or cross relationships between geochemical boundaries and gravity, Moho and magnet gradisnts. 地球化學邊界的形成與板塊的斜結合以及結合以後岩石圈結構調整產生的克拉通邊界密切相關。
- The relationship between Moho swell and modern morphological feature appear the mirror plane. 松遼前寒武古陸塊 (含開魯坳陷 ) ,是大中型移置體 ;
- 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. 在蘇中、蘇南、浙西、皖南地區,莫霍面與磁性基底升降大體一致。
- 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. 本文利用人工地震測深和天然地震資料反演得到莫霍面深度的數據給出了研究區內莫霍面的等值線圖。
- The Bouguer gravity anomaly in Tibetan Plateau is decomposed by wavelet transform and low-pass filter respectively,and applied to the inversion of Moho. 分別採用小波變換和低通濾波對青藏高原地區布格重力異常進行了位場分解和莫霍面反演,並將反演結果與地震資料作比較。
- 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. 本文利用三維廣義反演技術對重力資料進行反演，計算出了琉球溝弧盆系地區的莫氏面深度。
- The inversion results demonstrate that the Moho depths of Qinghai-Tibet plateau are shallow around the edges, and deep at the center. 結果表明，青藏高原莫霍面呈現出邊緣淺、中部深，邊緣變化快、梯度大，中間變化梯度趨緩的特點。
- Characteristics of Moho is significant to deep structures in East Sea because Moho is important density inference between Crust and Mantle. 莫霍面是地殼和上地幔的分界面,是個重要的密度界面,東海莫霍面的展布特徵,對於研究東海深部構造具有重要意義。
- The inversion results demonstrate that the Moho depths of Qinghai-Tibet plateau are shallow around the edges,and deep at the center. 結果表明,青藏高原莫霍面呈現出邊緣淺、中部深,邊緣變化快、梯度大,中間變化梯度趨緩的特點。
- The velocity structure features of sediment, basement, upper crust, lower crust, Conrad and Moho interfaces were analyzed. 分析了沉積層、基底、上地殼、康臘面、下地殼和莫霍面的特徵。
- 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. 本文對天山南麓1:100萬、1:50萬和1:10萬布格重力異常圖及相應的垂直磁力異常圖進行了處理,並計算了莫霍面深度。
- 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反射波探測了雅魯藏布江北側局部地區莫霍面的深度和起伏。
