喜马拉雅

The forming of the Himalayas-Yarlung Tsangpo orogenic belt occurred prior to the Miocene and therefore it can be confirmed that during the Paleogene there must have been a high convergence rate occurred between India and Eurasia.

发生在古近纪的日本海和中国的松辽盆地的弧后扩张与喜马拉雅山一雅鲁藏布江造山带的重力垮塌作用可以对比，可能是太平洋和欧亚大陆汇聚速率的突然减小造成的。

The study of dynamic evolvement course of Yarlung Zangbo River (the parallel water system on back edge of collided strap) on Himalayan block boundary and response to structure action is a bran-new angle.

研究喜马拉雅板块边界上雅鲁藏布江在板块边界上的动态演变过程及对构造活动的响应是一个全新的研究角度。

Much of what is being said fails to recognise the patchiness of past research in space and time, and a nearly-total absence of glacier monitoring at elevations where the most critical ice and climate changes occur.

鉴于更广大的喜马拉雅地区的复杂性和多样性，我们还必须运用科学和信息系统以及地区合作的手段。下面是一些新的研究计划提出的一些实用性建议

The data from sediments, tectonic and erosion rate show that this original peneplain was formed in the end of the Oligocene Epoch, a long crust steady phase after the first episode of Himalaya tectonic movement.

这个古老的原始夷平面形成于渐新世末，即喜马拉雅还动第一幕－冈底斯运动之后的地壳长期稳定时期，与青藏高原山顶夷平面以及华北北台期夷平面形成时间相当。

Situated at an altitude of 8,250 ft in the Himalayas , the Wildflower Hall presents a picture of breathtaking natural beauty.

在一个8250英尺的喜马拉雅山脉海拔的酒店野花厅提出了令人惊叹的自然美景图片。

It reveals that leucogranitic magma activity at least lasts to Pliocene Epoch in central segment of Higher Himalayan crust.

在聂拉木地区获得了6.23Ma浅色体形成年龄(这是目前在高喜马拉雅中段获得的最年轻的花岗岩浆活动的年龄资料)，标志着该地区的岩浆活动至少持续到上新世。

The floristic characteristics of the Xizang pteridophyte flora in relation to the upheaval of the Himalayas.

西藏蕨类植物区系的特点及其与喜马拉雅隆升的关系。

Qomolangma, the serene Holly Mountain of Tibetans, is still known to the world as Mt.

然而，这座喜马拉雅山的主峰仍然在为强加给她的错误名称而呻吟，因为国际社会至今还没有为她伸张正义。

Analyses of the sedimentary textures and structures, ecological features of the faunas, stratigraphic distribution and occurrence environment of radiolarian cherts indicate that the Weimei Formation belong to littoral-neritic sediments as is the case with the quartz sandstone at the top of the Menkadun Formation deposited synchronously with it.

对维美组的沉积结构，构造，动物群生态特征，地层展布情况和放射虫硅质岩的产出环境等进行了分析，认为维美组与其南部的同期沉积门卡墩组顶部石英砂岩一样，同属典型的滨浅海沉积，晚侏罗世康马-隆子和北喜马拉雅地层分区为统一的滨浅海，不存在次深海—深海环境。

Such, all goods and materials that carry China want from Indian north airborne, cross inland of China of the Himalayas reentrance, this calls at that time namely " hump is airborne ", but this airborne circuitry however very in a extremely dangerous state.

这样，所有运送到中国的物资都要从印度北部空运，越过喜马拉雅山再进入中国内陆，这就是当时称作的"驼峰空运"，但是这条空运线路却极为凶险。

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。