查询词典 Himalaya

Himalaya Sherpas, Nepal As two Sherpas cross a pole, National Geographic Expeditions members sit on the rocks below.

意译：喜马拉雅夏尔巴人，尼泊尔。作为两个夏尔巴人跨一极，国家地理探险队的成员坐于岩石下面。

As a glaciologist—he was an author of the relevant chapter in the WG-I report, a much more thorough take on the subject which makes no grandiose claims about the Himalaya—he found the passage absurd, and alerted the IPCC.

作为一名冰河学家，他发现这篇文章的荒谬并警告了IPCC。同时，他也是第一工作组报道相关文章的作者之一，对喜马拉雅山脉没有做宏大声明的项目更加彻底。

Himalaya, which formed on the basement of the Pan-African orogenic event at about 550 Ma BP and experienced Ordovician to Devonian platform sedimentation, was transformed into to a back-arc extensional-rifted zone at the end of the Carboniferous. The Yarlung Zangbo ophiolitic mélange zone is a Mesozoic back-arc spreading basin corresponding to the Gangdise paleo-island arc zone on the south side of the Tethyan Ocean. The Gangdise zone experienced island-arc orogeny in the Late Paleozoic. The very significant differences in geology on both sides of the Bangong Co-Nujiang suture zone suggest that the suture zone is not only the northern boundary of Gondwanaland and the boundary between the Indian (Yunnan-Tibet) stratigraphic realm and the South China (Qiangtang-Sanjiang) stratigraphic realm, but also the relics of subductional collision and final extinction of the Phanerozoic Tethyan Ocean after the breakup of the Neoproterozoic supercontinent Rodinia. The basic point of study of the collisional orogenic processes of the plateau is the structure and composition of the archipelagic arc-basin tectonic realm of three different stages bounded by three rigid paleocontinental blocks (Gondwanaland, Laurasia and Pan-Cathaysian) and the mutual constraining, transformation and coupling of various material movement forms.

喜马拉雅奠基于5.5亿年左右的泛非造山事件基底上，历经奥陶纪至泥盆纪台地沉积，并于石炭纪末转化为印度板块北缘的弧后伸展裂陷带；雅鲁藏布江蛇绿混杂岩带曾是特提斯大洋南侧与冈底斯古岛弧带相对应的中生代弧后扩张盆地；冈底斯带曾经历了晚古生代岛弧造山作用；班公湖-怒江带两侧大量地质特征重大差异表明，班公湖-怒江带是冈瓦纳大陆北界，是印度地层区和华南地层区的分界，是新元古代Rodinia超大陆解体后显生宙特提斯大洋俯冲，消减，碰撞，最后消亡的遗迹。

In Yadong district in central Himalaya, a retro-metamorphic high-pressure granulite and its country rock were focused and...更多 conventional 40Ar/39Ar tests were done.

在喜马拉雅造山带中东段，系统的针对岩体热史演化的研究尚处于起步阶段，喜马拉雅山的隆升之谜也一直没有彻底解开。

The Yoga origins from India, before the fable five millenniums on the ancient India's Mary mountain, some people build the sage, also some people become the gymnosophist, they will practice the secret to pass on the mean pursuer, the Yoga sustainer start only then the small number of people, generally in the temple, the village booth, the Himalaya Mountains cavern and the cover forest heartland will repair holds, will teach the disciple by the Yoga teacher who will be willing to accept for these.

瑜珈起源于印度，传说五千年前古印度的圣母山上，有人修成圣人，亦有人成为修行者，他们将修炼秘密传受给有意追求者，瑜珈维持者开始只有少数人，一般在寺院、乡间小舍、喜马拉雅山洞穴和茂密森林中心地带修持，由瑜珈师讲授给那些愿意接受的门徒。

The leucogranites veins occurred widespreadly in the para-metamorphic rocks, in which the hypersthene melagranulite distributed. That suggests the source rocks of leucogranites of the High Himalaya are para-metamorphic rocks. For the basement was uplifting, pressure relieved and lacked water, source rocks were melting partly and formed the leucogranite magma.

基底副变质岩中广泛分布淡色花岗岩脉体，在基底副变质岩中的淡色花岗岩脉体中发现紫苏辉石暗色麻粒岩残留体，这表明本区高喜马拉雅淡色花岗岩源岩为基底副变质岩，且基底副变质岩是在基底快速隆升降压的条件下发生缺水熔融生成的淡色花岗岩岩浆。

Coward M P, Butler R W H. Thrust tectonics and the deep structure of th e Pakistan Himalaya. Geology, 1985,13: 417～420

3青藏高原北缘的祁连山以双向逆冲形式挤出，南北两侧地块俯冲到祁连山下。

But more than 70% of the Zangbo , the main stem, is generated south of the Himalaya, so it would not greatly affect India.

但是其主干道雅鲁藏布江的70%，都发源于喜马拉雅山南部，因此这不会对印度产生太大的影响。

Through the research in recent years, this paper put forth a fire new notion about Himalaya n tectonic metallogenetic domain.

通过近年来的研究，提出了全新的喜马拉雅构造-成矿域概念。

The records of 56 stations in Himalaya area were analyzed by using the method of minimizing the eigenvalue. Shear wave splitting was observed in thirty-nine stations of them.

利用最小特征值法，分析了喜马拉雅地区56个台站的地震记录，其中有39个台站能观察到S波分裂，其平均分裂时间在0.8s左右。

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。