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Silicons are the most in the earth's crust, silicon oxidize the silicon form and exist by two more, is rich in two high-temperature karst which oxidize the silicon, under the function of the pressure, and soak trunks outside gradually inside, there is a crystallization course, it is the silication course.

地壳中硅是最多的,硅多以二氧化硅形式存在,富含二氧化硅的高温岩溶,在压力的作用下,从外及内逐渐浸润树干,并有个结晶过程,便是硅化过程。

The distinctive features of volcanic rocks, especially the spilite, illustrates that mantle plume or hotspot with small scale might be the essential origin of a series geologic events such as the extension of crust, the interval eruption of submarine bimodal volcanic rocks especially the increasing eruption of basic rocks, and the mineratlization of Ashele mine

认为成岩、成矿背景属裂陷拉张环境,火山岩尤其是细碧岩具有五大特殊性,初步提出了热点作用是导致地壳拉张、双峰式火山岩间互喷发、从早到晚基性火山作用趋于增强、以及成矿作用等一系列地质事件的深层次原因的看法

This dramatic range, steeper than the Himalayas, is the upturned rim of the eastern edge of Tibet, a plateau that has risen to 5 km in response to the slow but un stoppable collision of India with Asia that began about 55 million years ago and which continues unabated today.

这一引人注目的地域范围,比喜马拉雅山更加陡峭,是处于西藏东部边缘的朝上翻的边框地带。响应启始于约5500万年前的、缓慢的但却不可阻挡的印度与亚洲地壳板块碰撞,高原已上升至五千米,这种碰撞持续至今,毫无衰退。

The Paleoproterozoic Beidahe Group-complex remains as continental shivers in the interior of the North Qilian orogen. In its early stage of development, there occurred abundant amphibolite. The protolith of the amphibolite is basalts. The Alk-∑FeO-MgO plot, REE features and Rittmann index show that the protolith belongs to the calc-alkaline suite and exceptionally shows the subalkaline character. The rock is characterized by higher Al2O3 and ∑FeO and lower Mg#, indicating that it has a higher degree of compositional evolution and that the formation of volcanic rocks is related to activation of older crust. Highly fractionated REE patterns and amphibolite on the Ti-Zr-Y plot, Ni-FeO/MgO plot and Ta/Yb-Th/Yb plot all indicate the characteristics of volcanic arcs and active continental margins. On the geochemical diagram of basalt, the overall REE features are in the main analogous to those of calc-alkaline island-arc basalt, with Sr87/Sr86=0.71617–0.72033,Nd143/Nd144=0.512414–0.512495 and εNd=–2.79 to –4.37,εSr=245.78–305.3, showing that the magma was derived from the crust or subjected to contamination with the lower crust below the continent.

提要:以大陆碎块形式残存于北祁连造山带内部的古元古代北大河岩群早期发育有大量的斜长角闪岩,其原岩为玄武岩,Alk—∑FeO—MgO图解,REE特征,里特曼组合指数等均显示斜长角闪岩属钙碱性系列范围,个别显示弱碱性,斜长角闪岩具有较高的Al2O3,∑FeO和低的Mg#,这些特点反映其成分演化程度较高,表明火山岩的形成与古老地壳的活化有关,有较强分异的稀土元素分配模式,在Ti—Zr—Y图,Ni—FeO/MgO图解和Ta/Yb—Th/Yb图解上斜长角闪岩均显示火山弧或活动大陆边缘的特点,在玄武岩的地球化学形式图,稀土元素整体特征与钙碱性岛弧玄武岩基本相同;87Sr/86Sr=0.716 17~0.720 33, 143Nd/144Nd=0.512 414~0.512 495,εNd=-2.79~-4.37。

The stress system appears to be caused by fluid movements in the crust or subcrust.

应力系统似乎是流体运动所造成的地壳中或subcrust 。

The stress system appears to be caused by fluid movements in the crust or subcrust.

压力系统似乎由于流体运动在地壳或subcrust。

Some basic geological problems related to establish the Surficial Crust Section, such as the division of geomorphologic type and Quaternary time-genesis series, were also studied in detail.

一些与建立地壳表层断面有关的基础地质问题,如区内地貌类型的划分、第四纪堆积物时代-成因系列的建立等,也在文中做了详细的研究。

The Surficial Crust Section and Human-Earth relationship were treated separately as the main resear...

本文以地壳表层断面为主要研究对象,以人-地关系为主要研究内容。

The flow zone starts from the mid plateau, goes clockwise around the Eastern Himalayan Syntaxis, and ends at the southeast corner of the plateau with a fan-like front, which implies that the flow zone could be attributed to the escape of highly plastic upper crust material driven by gravitational buoyancy and lateral compression.

这一流滑带的前缘速度场在青藏高原东南角呈现出典型的扇形发散特征,表明整个流滑带可能起因于高塑性上地壳物质在挤压和重力共同作用下的连续性侧向逃逸。

Prestack migration method presented in this paper should be developed to apply in observational teleseismic P waveform data, to study the inhomogeneity of crust and upper mantle.

对本文所提出的接收函数叠前偏移方法作进一步的发展,可以用于实际的远震体波波形数据,在揭示地壳上地幔结构的横向非均匀性研究中,具有颇为广阔的应用前景。

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