莫霍面,Moho
1)Moho[英]['m?uh?u][美]['moho]莫霍面
1.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
2.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
3.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。
英文短句/例句

1.(5) Moho has complex change in research zone;(5 )研究区莫霍面具有较为复杂的变化 ;
2.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。
3.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。
4.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
5.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
6.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
7.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.
8.GRAVITY VARIATION AND MOHO SURFACE DEFORMA-TION BEFORE AND AFTER 1976 TANGSHAN EARTHQUAKE1976年唐山地震前后的重力变化和震区莫霍面的变形
9.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
10.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。
11.South of the Red River fault belt, the crustal structure is featuring approximately a two-layered velocity model as the dominent factor, and Moho surface deepens from south to north and the crust thickens from 37-40km.红河带以南,地壳结构近似于以两层模式为主,莫霍面南浅北深,壳厚37—40公里。
12.Mohorovicic Discontinuity (Moho)莫霍〔洛维奇〕不连续面;莫霍〔洛维奇〕界面
13.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
14.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
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.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.
17.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
18.mohoroviris discontinuity莫霍洛维奇不连续性
相关短句/例句

Moho discontinuity莫霍面
1.A Review on the Moho Discontinuity beneath the Tibetan Plateau;青藏高原莫霍面的研究进展
2.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。
3.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)。
3)Moho depth莫霍面
1.Moho depth and sedimentary thickness in Capital region;首都圈地区莫霍面起伏及沉积层厚度
2.In this paper, we use the teleseismic receiver function to determine the Moho depth and the one dimension velocity model under Xi′an Seismic Station.以西安地震台1992年至2000年记录到的853个远震宽频带数字地震记录为基础,利用远震接收函数的方法反演了西安地震台台基的一维速度结构及莫霍面深度,结果表明,西安地震台下的莫霍面深度为39。
3.The obtained Moho depth,crustal structure thickness,and Cenozoic and Mesozoic basement show that the formation mechanism of Mesozoic basins is different from that of the Cenozoic basins.利用OBS资料作约束条件对南海东北部的地球物理资料,主要是重力资料和多道反射地震资料进行反演,获取比较理想的莫霍面深度、地壳厚度、中生代沉积基底面、新生代沉积底界面等地壳结构信息。
4)Moho surface莫霍面
1.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。
2.Using the formulae, data of gravity measurement and leveling survey in the Hexi region of Gansu province and northwestern Yunnan province are computed, for study on variations of the lower crustal interface density and vertical deformation of Moho surface with time.根据计算结果 ,分析了 2个地区莫霍面密度变化速率和垂直形变速率与地震的关系 。
5)Moho[英]['m?uh?u][美]['moho]莫霍界面
1.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。
2.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。
6)series and tpyes of granitiods莫霍面图
延伸阅读

莫霍界面莫霍界面地壳和地幔的分界面。1909年A.莫霍洛维奇根据对克罗地亚的地震图的分析,识别出这一界面的存在,根据发现者的名字命名。又称莫霍洛维奇间断面。见地球内部构造。