1.
GRAVITY COMPENSATION OF THE MOHOROVICIC DISCONTINUITY AND THE BASIC MODEL OF CRUSTAL STRUCTURE
莫霍界面的重力补偿和地壳结构的基本模式
2.
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.
3.
Moho Depths beneath Broad-Band Stations in Fujian Area Inversed by Teleseismic Receiver Function
用远震接收函数反演福建地区宽频带台站下方莫霍界面深度
4.
The crust and mantle are separated by a seismically determined boundary known as the Moho-discontinuity.
改译为：地壳与地幔的交接处系根据地波走失而确定的一个界面,通称为莫霍界面。
5.
Mohorovicic Discontinuity (Moho)
莫霍〔洛维奇〕不连续面；莫霍〔洛维奇〕界面
6.
(5) Moho has complex change in research zone;
(5 )研究区莫霍面具有较为复杂的变化 ;
7.
The Mohole and Conrad are calculated, showing the characteristics of the deep northwest and the low southeast.
计算得出的莫霍面及康氏面均为西北深,东南浅。
8.
The uplift-depression of the Moho is rather gentle with a maximum of 5～6 kilometers.
莫霍面升降梯度较缓,最大幅度在5～6公里以内。
9.
A DISCUSSION ABOUT THE RELATIONSHLP BETWEEN MOHO FORM AND SPATIAL DISTRIBUTION OF LARGE ORE DEPOSIT IN YUNNAN
云南莫霍面形态与大型矿床空间关系探讨
10.
RESEARCH OF MOHO BASIC FEATURES ON EASTERN QINLING DEEP SEISMIC PROFILE
东秦岭深地震剖面上莫霍基本特征的研究
11.
The Moho Depth of Qinghai-Tibet Plateau Revealed by Seismic Detection
由地震探测揭示的青藏高原莫霍面深度
12.
The Moho Depth of South China Revealed by Seismic Probing
深地震探测揭示的华南地区莫霍面深度
13.
We pick up the instantaneous information of Moho phase in typical segment of the profile.
对典型剖面段的莫霍面震相进行瞬时信息的提取.
14.
GRAVITY VARIATION AND MOHO SURFACE DEFORMA-TION BEFORE AND AFTER 1976 TANGSHAN EARTHQUAKE
1976年唐山地震前后的重力变化和震区莫霍面的变形
15.
The exterior portion of the earth that lies above the Mohorovi錳 discontinuity.
地壳位于莫霍洛维奇契不连续面之上的地球外层
16.
CHARACTERISTICS OF SEISMIC VELOCITY STRUCTURE OF THE CRUST AND UPPER MANTLE AND MOHO DISCONTINUITY IN GULEI-SHICHENG AREA
古雷—石城地区地壳与上地幔地震波速度结构及莫霍面特征
17.
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。
18.
mohoroviris discontinuity
莫霍洛维奇不连续性