We should especially notice that there is a near NE trending crustal thickness abrupt variation beltat the depth of Moho in the region, which cuts across the west of Tianchi and corresponds to Ma'anshan-Sandaobaihe graben fault. The fault belt may have played an important role in the migration of magma as the volcano erupted.
特别值得注意的是，存在着一条近北东方向的莫霍面深度陡变带从天池火山口西部穿过，相应位置与马鞍山—三道白河地堑型断裂相一致，该断裂带可能对天山火山喷发时岩浆的运移起到重要作用。
In the development of Earth Science, scientists pay more attention to the research of Moho.
在地球科学发展中，莫霍面的研究进展备受关注。
Moho surface is the interface of crust and upper mantle and is an important density interface.
莫霍面是地壳和上地幔的分界面，是一个重要的密度界面。
In this paper, the authors have summarized the results of the detection work, and discussed the Moho variation in Northwest China.
本文通过对西北地区的深地震探测研究的总结和梳理，探讨了西北地区的莫霍面深度与变化及其地球动力学意义。
In this paper the authors summarize these detections, then discuss the Moho variation in NW China.
本文通过对西北地区的深地震探测研究的总结和梳理，探讨了西北地区的莫霍面深部与变化及其地球动力学意义。
The complicated region in structure with large depth and overlap Mohoconverters is just about the modern seismic activity belt. The depth of the structureactivity belt is about 100km.
天山的Moho面加深、重叠等构造复杂段正是现代地震活动带，说明该段的构造活动还在继续进行着。
Moho is a east inclined surface tending to NNE., and the thickness of the crust reduces from 21 km to 18 km.
莫霍面为一北北东向的向东倾伏的幔坡，地壳厚度由21 km减至18 km。
Then we invert both the depth of Moho discontinuity and upper surface of low density layer in the top of the upper mental using multiply layers inversion method.
本文通过正演计算剥去浅部沉积层的影响，然后利用多层密度界面反演方法，同时反演莫氏面深度和异常上地幔顶界深度。
The gravity anomaly can be well simulated only by placing a huge low-density body from the surface to the Moho at the boundary between the North and the South Dabie Mountains, at the root of the Dabie Mountains.
只有将位于大别山山根上，南北大别之间设置一个从地表直达莫霍界面的巨大低密度体，重力曲线才能得到很好的拟合。
Bouguer gravity anomaly in North China is decomposed with multi-scale decomposition technique of wavelet transform, and gravity anomalies produced by anomalous density bodies of varying scales from surface to Moho are revealed.
采用小波变换多尺度分解技术，对华北地区布格重力异常进行分解，获得自地表至 Moho界面深度范围内不同尺度的密度异常体产生的重力异常。
This paper probes into some difficult problems about geothermal field simulation of basins and their solving method:(1) From the angle of equilibrum and wreck of underground thermal state, the authors adopt the concepts of normal geothermal field and appended geothermal field to describe the contribution of normal crust-mantle convection to the geothermal field and the contribution of magmatic intrusion to geothermal field respectively; (2) The authors try to discuss the method of gaining the thermal flow value about basin bottom, that by using analyzing paleo-geothermal structure, and also try to discuss the availability of empirical formula for burial depth of Moho surface which is established on the basis of the relationship of inverted image between basin bottom and Moho surface in gravity compensated area; and (3) Based on the relation curve among thermal conductivity, lithologic characters and earth temperature provided by Ungerer etc, the authors establish an empirical formula about the thermal conductivity of rock through double regression.
作者从地下热流状态平衡与破坏的角度出发，用正常地热场的概念来描述常规上地幔热流对地热场的贡献，而用附加地热场的概念来描述岩浆侵入等事件对地热场的贡献；讨论了采用地壳热结构分析来获取盆地基底热流数值的方法，以及根据重力补偿地区的盆地基底与莫霍面的倒影关系所建立的莫霍面埋深经验公式的有效性；以Ungerer等提供的岩石热导率与岩性、地温之间的关系曲线为基础，采用双重回归方法建立了岩石热导率的经验公式。
Based on the mapping of the granitic series and types, strontium isotopic trend surface analyses and isobaths of Moho surface, the deep-level sourced Yangtze series granitoids are mainly distributed in the eastern part of South China.
根据花岗岩系列和类型编图，华南地区浅源南岭系列花岗岩多產於中部和西部，深源长江系列花岗岩主要分佈在东部。
Especially the Moho discontinuity between the earth's crust and mantle, the Gutenberg discontinuity between the mantle and the core, and the gradational change between the outer and inner core.
特指地壳和地幔之间的莫霍不连续面，地幔和地核之间的古登堡不连续面，以及外地核和内地核之间的渐变面。
Totally, 21 earthquakes have been relocated at depth of 50~80 km which was very near the Moho.
发现区域震源深度呈明显的双层分布，其中有21 个地震的深度在50～80 km之间，与该地区的莫霍面深度相近。
It is generally accepted that the moho depth is about 30~39km in this region.
认为：该区莫霍面深约为30～39km.410km的间断面有30km的深度异常，这种异常是否在过渡带正常或含水相变展布厚度的内，还是于该区俯冲带的后退有关，还需做进一步的研究论证。
Spanish firm Moho Architects are currently in the schematic design phase of a mixed use tower for San Jose, Costa Rica.
西班牙Moho建筑事务所最近为哥斯达黎加的圣何塞设计了一个多功能塔楼，这是它的示意图。
In terms of gravity and magenetic anomaly data, we have studied the features of the Moho and Conrad discontinuit as well as the structures of density and magnetism over the Tarim baisin.
根据重力和磁力资料分析，研究了塔里木盆地的莫霍界面和康氏界面深度分布特征及地壳上地幔的密度和磁性结构。
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。
The fine seismic velocity structure, electrical conductivity structure and geometrical construction of the crust in Shanghai region and the coupled relationship between the deep and shallow structures are investigated by using multi-geophysics exploration methods, such as shallow seismic reflection, deep seismic reflection, high-resolution seismic refraction, deep seismic wide angle reflection/refraction and magnetotelluric sounding.
通过在上海地区开展深、浅地震反射、地震宽角反射／折射、高分辨地震折射和大地电磁测深等联合剖面探测，获得了该地区近地表至Moho面的精细速度结构、电性结构和深浅构造关系。
Relation between the Granite Series and Types, Strontium Isotope Compositions and Isobaths of Moho Surface in South China: Distirbution of Granite Series/Types Restricted by the Analysis of Strontium Isotopic Tendency Surface and the Depth Variation of Moho Surface
华南花岗岩分类与鍶同位素和莫霍面的关係：花岗岩系列／类型分佈与鍶同位素趋势面分佈和莫霍面深度变化的制约，王联魁；王谦身；徐文新；陈根文；张绍立-66文免费论文库，大学生论文库