Airry isostatic anomalies and Moho-depth were calculated and analysed.
研究了该剖面及其邻区为主的青藏高原西北边缘重力场特征；划分了３个地质构造单元及８条较大断裂；计算并分析了Ａｉｒｙ重力均衡异常及莫霍界面深度。
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 residu- al anomalies.
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。
Moho Depths Inversion of Qinghai-Tibet Plateau with Variable Density Model;
用变密度模型反演青藏高原的莫霍面深度
The Study on the fluctuation of Moho in Yellow Sea and its adjacent area;
黄海及邻区莫霍面起伏特征
It is confirmed that Jiyang depression of Paleogene occurred in trans-extensional behavior in the light of Moho uplifting,lithosphere thinning,development of basic and ultra basic igneous rocks in mantle source rocks,high geothermal gradient,halfgraben-like depression bas.
从8个方面(莫霍面上隆和岩石圈减薄、幔源基性火山岩和超基性岩的发育、高的地温梯度、一系列箕状断陷盆地群的伸展量高达50km以上及沉积速率高达0。
A Review on the Moho Discontinuity beneath the Tibetan Plateau;
青藏高原莫霍面的研究进展
The infrastructure of this zone is apparently controlled by the transitional belt between the mantle slope of Yunyang backbone and the mantle flat of Xunyang on Moho discontinuity and by the western marginal rim of Wudang platform on Conrad discontinuity.
该矿带在深层构造上明显受莫霍面郧阳脊状幔坡与旬阳幔坪之间的过渡带和康拉德面武当坪台西部边缘的控制。
Some new viewpoints were proposed concerning the trend and extension of the southwestern end of the Altun strike-slip fault,the origin of two low gravity zones was discussed,the altitude of the Moho discontinuity in the .
对阿尔金走滑断裂西南端的走向和延伸提出了一些新的看法;讨论了2条重力低值带的成因;推断了班公湖—怒江结合带下部莫霍面隆起的高度,从重力角度提出了对班公湖—怒江结合带的认识;认为青藏块体在拼合后地壳有2个加厚中心;新圈定了一个中、新生代沉积盆地,并进行了初步研究;结合地质、矿产、航磁等资料,初步划分出4个成矿远景区(带)。
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
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.
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
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。
Mohorovicic Discontinuity (Moho)
莫霍〔洛维奇〕不连续面；莫霍〔洛维奇〕界面
(5) Moho has complex change in research zone;
(5 )研究区莫霍面具有较为复杂的变化 ;
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。
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。
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
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
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
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
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.
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
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
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
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。
mohoroviris discontinuity
莫霍洛维奇不连续性
