moho
- 网络莫霍面;莫霍;莫霍界面
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Relationship between Moho shape and distribution of rock gold deposit in China
中国莫霍面形态与岩金矿分布关系
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Moho Pattern and Deep Structure in the North Centre of South China Sea
南海中北部莫霍面及深部构造
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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
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The Moho depths are quite different in different tectonic element .
不同的构造单元莫霍面深度有明显的不同。
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Three deep faults cutting the Moho discontinuity are also exhibited .
在深部可能有三个错断莫霍面的断裂带。
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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
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Structure of Moho in North china & 3-d inversion from deep seismic sounding data
华北莫霍面构造形态&深地震测深数据的三维反演
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Deep fault zones are represented by variation sites of Moho surface .
莫霍面变异部位多为深断裂带反映。
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The general features of the Moho are obtained mainly based on artificial seismic sounding data ;
2主要利用人工地震测深资料得到莫霍面的基本特征;
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Their spatial distribution has some bearing on the Moho .
它们在空间分布上与莫霍面有一定关系。
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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
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The development of studies on Moho using near - vertical seismic reflection in recent years is introduced .
概述了近年来用近垂直反射地震技术研究莫霍面的进展。
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Moho has inner structure and can be found all over the continent .
莫霍面几乎遍布全国,它具有内部结构。
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Depth Distribution of Moho Discontinuity beneath the Beijing and Its Adjacent Area
北京及邻近地区Moho面的深度分布及其构造意义
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An analysis on the shape and genesis of the Moho in Tianshan
天山莫霍面的形态及其成因分析
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Using gravitational and magnetic data of the area we calculated Moho and Courier interfaces .
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。
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Trial discussion on the form of Moho discontinuity and crustal thickness of Hunan Province
试论湖南省莫霍面形态及地壳厚度特征
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Undulation of Moho and Ductile Flow of Lower Crust Induced by Mantle Flow
地幔对流诱发的莫霍面起伏与下地壳塑性流动
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The structure and fluctuation of Moho as well as the distribution of the faults are also discussed in the paper .
此外,还讨论了莫霍面结构,界面起伏和断裂展布概况。
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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。
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Calculation of the Moho discontinuity and discussion of feature of gravity field in the Antarctic region
南极重力场特征及界面的计算与解释
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There still are observed reflections beneath the Moho discontinuity .
Moho以下仍有反射信息。
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This paper also discusses the deep regional anomaly , presumably resulting from the rise of the Moho surface .
同时又探讨了第三类深部区域异常,推测其可能是莫霍面隆起所致。
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The distribution of the crystalline basement has a symmetrical relation with the Moho .
结晶基底的展布形态与地壳底界,即莫霍面呈近似镜像对称。
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The depth of Moho - surface was calculated by Parker-Oldenburg inversion .
应用Parker-Oldenburg法反演计算了莫霍面深度。
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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
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Seismic P_n waves sample the top of the upper mantle right beneath the Moho .
Pn波是通过莫霍面下方的上地幔顶部的地震波。
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And ③ the characteristics of the crust structure have been analyzed by using the data of the magnetic basement and Moho .
利用磁性基底和莫霍面数据分析本区地壳结构特征。
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Correction to the Moho discontinuity depth of the northwestern China using the data of seismologic tomography
利用地震层析成像数据修正中国西北地区莫霍界面深度
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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。