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Moho相关的网络例句
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This paper proposed the method and technique of the inversion of Moho depth of China and adjacent areas according to Bouguer gravity anomaly.

提出应用布格重力异常反演中国海陆莫霍面深度的方法与技术,并考虑到中国海、陆构造的一体性,进行海陆统一编图以展示莫霍面的海、陆演化与构造关系。

We have calculated the Bouguer gravity anomaly from its the free-air gravity anomaly and then get the depth of Moho-depth.

由自由空间重力异常值计算布格重力异常值,再由布格重力异常值计算莫霍面的深度,由浅入深的研究渤海的构造。

There are intimate connection between the Bouguer gravity anomaly and the Moho depth, so it is one of main methods to inverse the Moho depth according to gravity anomaly.

布格重力异常与莫霍面深度之间具有紧密的联系,利用重力异常反演莫霍面深度成是研究莫霍面深度和编制莫霍面深度图的主要手段之一。

Analyze characteristics of Crust-Mantle and deep structures by calculating Moho buried depths with bouguer gravity anomaly and combing before results.

利用最新重力数据反演莫霍面埋深,结合前人的莫霍面埋深结果,分析东海的壳-幔结构及深部构造特征。

Compared with the result inversed directly by the Bouguer anomalies, this method yielded a correction of 6km for the Moho depth.

对比以前直接使用布格重力异常反演地壳厚度的结果表明,该方法对莫霍界面将产生6km的修正。

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。

The main study of this paper is about the properties and features of Moho. It is one of the two primo-velocity discontinuity and the nearest global interface to the obverse of the Earth. We can connect the phenomenon obtained with Moho Discontinuity, which is the principle facts to the existent environment of human being.

莫霍面作为地球内部的最明显的两个一级速度间断面之一,并且也是地球内部最接近地球表面的全球性分界面,与人类的生存环境关系最为密切,也是有可能与地表观察的结果相联系。

The 43-57km lithospheric mantle could be consist of a suite of cumulates with crystalloblastic texture, cumulate texture and relic magmatic crystalline textures, such as orthopyroxenite, websterite, clinopyroxenite and olivine-pyroxenite. The lithospheric mantle of 43km to Moho discontinuity could be spinel harzbergite and minor spinel lherzolite, in which the spinel harzbergite and minor spinel lherzolite xenoliths are discoveried. The Moho in the region could be an transitional zone composed of cumulates in petrology.

它既包括了具变晶结构的斜方辉石岩、二辉石岩,又包括了具有残留岩浆结晶结构与堆积结构的橄辉岩和辉石岩;向上至莫霍面,应为尖晶石方辉橄榄岩,并有少量尖晶石二辉橄榄岩,本区发现的尖晶石二辉橄榄岩(T7-21)和尖晶石方辉橄榄岩(T35、T58)可能来自该层;本区莫霍面在岩石学上可能为一个由堆积岩组成的过渡带(3~5km)。

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

The result shows that the crustal deformation is changing a lot in NW China: the deepest Moho is beneath the conjuction of west Kunlun and Karakorum, about 90 km deep, the shallowest Moho is beneath Jayir mountain to the west of Karamay, about 35.5 km; the Moho depth in the western segments of Tien shan is deeper then the mindle and eastern segments; there are Moho offset beneath Altyn fault, central Tien Shan northern margin fault and so on.

结果表明:比起我国其他地区,西北地区莫霍面无论是埋深还是形态均变化最大,反映出受印度板块与欧亚板块碰撞影响,西北地区地壳整体变形强烈。莫霍面最深(约90 km)位于西昆仑与喀喇昆仑构造结合处,最浅处位于准噶尔盆地西缘的克拉玛依(约35.5 km),最深与最浅差约55km。在盆山结合部位及大型走滑断裂,如阿尔金断裂、中天山北缘断裂带等均存在莫霍面错断。

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