Moho

The final model indicates that the thickness of the main part of Tarim basin varies in the range of 38~ 46 km. The model also reveals that the Moho dips southward beneath southern Tarim basin at an angle in concordance with the angle of the crystalline basement.

最终的模型显示塔里木盆地主体的地壳厚度为38～46km，而且塔里木南缘的Moho界面南倾，与结晶基底南倾的角度大体一致。

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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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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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The V shape coupling relationship between the basin and the range is located between the Tarim basin and the West Kunlun tectonic belt, just above the upwarped area of Moho.

塔里木盆地南缘与西昆仑构造带间呈V型盆山耦合关系，其下方恰好是莫霍面上隆区。

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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.

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Even further south, reflections from 35 km 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.

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Moho Depths beneath Broad-Band Stations in Fujian Area Inversed by Teleseismic Receiver Function Shaking table model test on Pudong International Airport Terminal 2 Building in Shanghai

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上海浦东机场T2航站楼结构模型模拟地震振动台试验研究

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Based on the comparative analysis and study on 10 profiles of telluric electromagnetic sounding ( MT) and regional gravimetric, magnetic data and Moho surface, the deep geological tectonic pattern of the central southern Jiangxi is discussed in this paper.

通过对江西省10条大地电磁测深（MT）剖面研究成果和区域重磁、莫霍面对比分析研究，讨论了赣中南地区深部地质构造格架。

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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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The Moho discontinuity on the Tarim side is distinctly imaged sub-horizontally at depths of~ 44 km.

塔里木盆地的Moho界面非常清楚，近水平地位于~44km深度上。

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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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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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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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Nowadays the wide angle reflection/ refraction-the deep-crustal sounding is usually used as a seismic method in the world mainly for Studying rough structure of Moho& its overling beds.

目前世界上用地震方法研究地壳结构，通常借助于广角反射或折射，即地震地壳测深方法，研究对象主要是莫霍面及其上覆层的粗略结构。

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The abyssal fault with high dip angle under the detachment surface cutting through the middle and lower crust to Moho is the causative fault for the Xingtai large earthquake, whose dislocation can cause strong earthquakes, shallow fault activity and the motion of surface material.

滑脱面以下存在的贯穿中、下地壳直至Moho面的高倾角深大断裂是邢台大震的发震断裂.它的错动引起大震，并引起浅层断裂的活动和地表土层物质的运动。

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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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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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Huoshan west-margin fault is perpendicular fault, and deeps down to the Moho discontinuity surface ( 38km).

霍山西麓山前大断裂的深部延伸为直立状，深度达莫霍面（38km）。

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On the relation between the lateral variation of velocities of p_n and the lateral difference of thermal regime at Moho

壳&幔侧面波（P n）速度的横向变化与界面温度横向差异的讨论

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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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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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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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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 thickness of upper crust is about 12 km, of middle crust is 9 km, of lower crust is 11 km. The depth of MOHO is about 32 km.

计算结果表明，本区上地壳厚约12km，中地壳厚约9km，下地壳厚约11km，Moho面深约32km。

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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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Below the Moho there is a crust-mantle transition zone with a layer velocity of 7.5 7.6 km/ s and a thickness of 22 29km.

上地幔顶部出现速度异常。西昌地区壳下存在一厚度为2228km，层速度为7.57.6km/s的壳幔过渡带。

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The reflection wave Pm on Moho discontinuity in 104-180 km is 7-10 times greater than Pg wave.

莫霍界面上的反射波P_ M在 140—180 公里范围比P_ g波 强10—7倍.

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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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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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