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The geodynamics processes of these deposits is related to the crust horizontal and vertical accretions. The eastern Tianshan domain has been the one of the most important metal deposits provinces in China.

上述矿床在形成过程中既有地壳的水平增生,也有地壳的垂向增生作用,已经构成了我国重要的内生金属矿床富集区。

This implies a major stage of crustal growth in Proterozoic time and remelting of the crustal material in Early Jurassic time;(5) The Oligocene-Miocene adakites contain magmatic zircons that show similar Hf isotope compositions to the Cretaceous-Paleogene Gangdese batholiths, providing a key constraint that allows evaluation of the nature and timing of crustal thickening in southern Tibet owing to the India-Asia collision; and (6) As a whole, the Hf isotope information observed in zircons from the above Transhimalayan rocks demonstrates a temporal variation in εHf values, and thus TDMC ages, that suggests multiple stages of orogenic or crustal formation events.

五、渐新世、中新世的埃达克岩,其岩浆锆石的铪同位素特徵与白垩纪、古第三纪冈底斯岩浆相似,因而为藏南在印亚碰撞以后,地壳增厚的时间与机制提供了关键性的制约;六、综观上述藏南火成岩中的锆石,它们与时变化的铪同位素初始值及其对应的模式年龄记录了拉萨地块多阶段的造山与地壳形成历史。

E The fractal and spherical particles exist favorably in the coarse fraction, while in the fine mode (0μm) are floccules formed by flocking fine particles together, containing crustal elements and mainly being silicates and aluminosilicates. f The content of Al, Si, Fe in TSP samples is higher than in PM〓, indicating an enrichment of these elements in coarse mode. g Compared with non-dust particles, the dust particles are more homogeneous in terms of morphology, particle size and composition. h Particles with irregular shape and well-distributed size dominate in dust samples, containing crustal elements such as Mg, Al, Si, Ca, Fe et al.

细粒中除小圆球外,大多为细小颗粒聚结在一起的不规则块状颗粒,主要含地壳元素,可能是硅酸盐和铝硅酸盐。fMg、Al、Si、Fe在PM〓中的含量较相应的TSP中的低,可见这些元素主要存在于较粗颗粒中。g沙尘期气溶胶粒子的形貌较非沙尘期单一、均匀,非沙尘气溶胶粒子的形貌、组分较沙尘期复杂。h沙尘期样品中,粒径均匀、形状不规则的颗粒最多,这些颗粒主要含地壳元素Mg、Al、Si、Ca和Fe等,是典型的由源区传输过来的沙尘粒子,但其高硫含量表明在青岛特殊的地理环境下,在粒子表面发生了硫的均相和非均相反应。

The granulite xenoliths, as the product of basaltic underplating and the representative of the present-day lower crust, are different from the local Archean granulite terrains There is a systematic variation of Sr-Nd isotopes from the granulites to the pyroxenites and the peridotites, indicating the possible crust-mantle interaction beneath Hannuoba area.

麻粒岩类捕掳体所代表的年轻大陆下地壳为玄武质底垫作用的产物,与麻粒岩地体所代表的古老大陆下地壳不同。橄榄岩类捕掳体则具亏损特征,辉石岩类捕掳体的性质介于麻粒岩类和橄榄岩类捕掳体之间,但石榴子石辉石岩显示了其特殊性。

However, t h e crust is almost four times t h icker t h an t h e eart h 's crust.

然而,月球地壳几乎是地球地壳厚度的四倍。

In recent year, the receiver function method has become an important method for inversing crustal thickness, whose main process is to use the travel time and amplitude difference between the direct P and P-to-S at Moho discontinuity to inverse the crustal structure and thickness.

近年来,接收函数已经成为一种重要的计算地壳厚度的产法,它是利用直达P波和Moho面转换S波震相的到时和振幅差来反演计算地壳的厚度和速度结构的。

The disturbing rields caused by the speedup and quietude of upper crustal movement in Tibetan Plateau indicate that, when the upper crust movement is speedup in Tibetan Plateau and keeps the boundary condition unchanged, the energy stored in upper crust is released, the driving force by Indian plate increases the horizontal compression stress and movement in other layers in Tibetan Plateau, and increase the horizontal compression stress in the whole geosphere in North China area Comparing the disturbing distribution of horizontal compression stress in the upper mantle layer, the value in North China area is only about one twelfths of that in south part of Tibetan Plateau.

3青藏高原地区地壳非均匀活动在中国大陆岩石层引起扰动场的研究结果表明,在保持板块边界作用强度不变的情况下,青藏高原地区岩石层上部地壳运动的增强,增加了其岩石层下部的向前推挤,同时也增加了对其它块体的推挤作用,以上地幔盖层内最大水平主压应力的扰动值为例,华北地区比青藏高原南部地区小一个量级。

The strike of Huanghai block and Huaihai block in the east mainly tends towards north-east, while the strike of Shanxi block and the eastern edge of Ordos block in the west mainly tends towards north-west.(3) According to the feature of Moho, the crust of the research zone can be divided into six parts in the Shanxi block, Moho looks like a nearly north-south sunk belt, and the crust is thick; at the southern edge of the Inner Mongolia block and in the south of Yanshan block, Moho presents the structural features of fold belt, tending nearly towards east-west; at the eastern edge of Ordos block, the structure of Moho is relatively complex with nearly northwest folds.

3根据莫霍面的形态特征,研究区地壳可大致划分为6个区块;在山西地块范围内,莫霍面呈近南北向的凹陷带,地壳厚度大;内蒙古地块南缘和燕山地块南部,莫霍面表现出褶皱带的构造特征,其延展趋势为近东西方向;鄂尔多斯地块东缘,莫霍面构造相对复杂,呈近北西向凸、凹相伴的褶皱;黄淮海地块为莫霍面隆坳区,隆、坳相间排列,构造较复杂,但从整体上看,这是全区莫霍面最浅的隆起区段;鲁西台背斜主要为莫霍面断陷区,其断陷带沿枣庄-曲阜一线向北西方向延伸。

And the Precambrian was a main period of the growth of the continental crust. Therefore the origin, formation and evolution of the continental crust and their model are some of the most important problems to which earth scientists pay close attention.

前寒武纪还是大陆地壳生长的主要时期,大陆地壳的形成、成因、演化过程及其模式是地球科学家最关心的问题之一。

To study the deep faults of crust through geophysics not only provides proofs to further study of basic theories such as the crust evolution and continent formation, but also provides an important guidance to classifying tectonic units, analysing and predicting natural earthquake activities and studying different kinds of mineralisation.

利用地球物理研究地壳的深部构造,不仅为地壳的演化和大陆的形成等基础理论问题的深入研究提供证据,而且对划分大地构造单元、分析和预报天然地震的活动性以及研究各种矿产的成矿规律也具有十分重要的指导意义。

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