地壳的

After studying the fault displacement distribution of Northern Linear Anticlinal Zone and Qiulitage Thrust Front, their mean crustal horizontal shortening rates are estimated as 37.1% and 36% respectively.

断裂位移场的研究表明北部线性背斜带平均地壳水平缩短率为37.1％，丘里塔格前锋带东丘里塔格段的平均地壳水平缩短率为36％。

However, the crust is almost four times thicker than the earth's curst.

然而，月球地壳几乎是地球地壳厚度的四倍。

The rock is peridotite, which is one of the main rocks in the upper mantle, an area that provides a girth below the Earth's crust.

这种石头是一种橄榄岩，是上地幔中的一种主要岩石。地幔位于地壳下面，包围着地壳。

There are two types of adakites with different petrogenesis: one type is formed by the melting of s...

埃达克岩存在两种成因类型：一种由俯冲的年轻(≤2 5～ 30 Ma)大洋板片熔融形成；另一种由增厚地壳环境中的玄武质下地壳熔融形成。

Results show that the Spiti shale in Zanskar terminated 15Ma later than that in southern Tibet, while the lowermost Cretaceous quartz sandstone in Zanskar appeared 18Ma later than that in southern Tibet. The age of volcanic sandstone in southern Tibet is very poorly time constraint and their deposition occurred somewhere within Berriasian～early Albian. In Thakkhola, the Chukh Group volcanic sandstone are of late Hauterivian-early Albian age (duration about 20Ma), while in Zanskar, the volcanic sandstones facies only appeared in Albian (duration of less than 10Ma). Therefore, it can be concluded that the onsets of both quartz sandstone and volcanic sandstone occurred earlier in eastern Tethys Himalayas than in western Tethys Himalayas .

侏罗纪末～白垩纪初印度大陆的北缘同时期存在大陆向上挠曲，导致陆源碎屑输入量的快速增加，石英砂岩广泛存在；早白垩世火山岩屑砂岩对应着的印度大陆北缘地层侵蚀加深，使得较深部的深成火山岩暴露并遭受侵蚀；石英砂岩和早白垩世岩屑砂岩所代表的印度大陆剥露时间在空间上的&东早西晚&，说明构造运动首先是从特提斯喜马拉雅的东部开始（大印度与澳大利亚的彻底分离），然后逐渐波及西部的，东西时间差为15～20Ma；由于地壳均衡作用，大陆分离后原先地壳挠曲转变为地壳下沉，发生强烈的构造沉降，故Albian之后沉积一套深水环境下的海绿石、磷酸盐和黑色页岩沉积。

Partial melting is not only an essential way to form granulitic lower crust, but also plays an important role on crustal deformation, reconstitution and adjustment of crustal textures.

部分熔融是形成喜马拉雅中下地壳麻粒岩的一种重要方式，并且在喜马拉雅造山带地壳变形、物质分异和调整过程中起着重要作用。

In the upper crust the fast wave directions follow geological trends. In the low velocity zones of lower crust and uppermost mantle, remarkable anisotrpy depicts the large-scale horizontal flow around east Himalayan syntaxis.

在上地壳内，快波方向与地表构造形迹基本一致；在中下地壳和上地幔顶部低速层内，各向异性非常显著，表明围绕喜马拉雅东构造结发生大规模的水平向流动。

The space between stations is about 3-20 km.The crust and upper mantle structure down to 100 km deep along our profile is obtained from our teleseismic waveform data in terms of the receiver function method.

利用记录的远震P波波形数据和接收函数方法，获得了沿剖面100km深度范围内地壳上地幔S波速度结构以及地壳上地幔一级间断面的形态。

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。

Overall, crustal thickness peaks in the Tibetan Plateau, decreasing in Tien Shan and its surrounding areas and thinning out in Southern China even thinner.

总体上看。青藏高原地区的地壳厚度最大，天山、准格尔盆地、内蒙古大部地区次之，中国华南沿海一带地壳厚度更小。

The labia have now been sutured together almost completely.The drains and the Foley catheter come out at the top.

此刻阴唇已经几乎完全的缝在一起了，排除多余淤血体液的管子和Foley导管从顶端冒出来。

To get the business done, I suggest we split the difference in price.

为了做成这笔生意，我建议我们在价格上大家各让一半。