蒙古

Forty-seven strains of bacteria were isolated from the samples of Kumiss products collected from the pastoral area in Xilin Guole,and its biological properties were studied.

本项研究主要以内蒙古锡林郭勒牧区马奶酒发酵菌冻干粉为样品，进行了马奶酒发酵菌的活化、分离、纯化、鉴定及其生物活性的研究。

A Tibetan or Mongolian priest of Lamaism.

西藏或蒙古喇嘛教的牧师。

Their religious beliefs, the Tuva and Mongolian Lamaism beliefs are the same, but also retain some of the relic Shamanism.

他们的长相和蒙古人很相似，而且服装服饰和生活习惯也基本一致。

A center of Lamaist Buddhism, Tibet first flourished as an independent kingdom in the seventh century.

是喇嘛教的中心，它最早作为一个独立王国在7世纪时处于鼎盛时期，13至18世纪处于蒙古控制之下，后来归为中国统治

Mongolia is located in the landlocked Central Asian country.

蒙古是位于亚洲中部的内陆国。

Transfecting efficiency of menggu sheep is 52%,Beijing duck is 23%,Qingyuan flesh chicken is 33%,zang chicken is 20%,langshan chicken is 19%.

转染率分别为蒙古羊52%、北京鸭23%、清远麻鸡33%、藏鸡20%、狼山鸡19%。

There apparently exist extensional deformation and layer parallel plane in Langshan group in the earliest stage.

对内蒙古霍各乞矿区内面理、线理、褶皱、断裂构造进行多层次、多尺度、详细的构造解析发现，内蒙古霍各乞矿区狼山群早期存在明显的伸展变形，广泛出现顺层面理。

Laster year,the Tsaatan learned that the goverrnment of Mongolia planes planned to spend one and a half million dollars on their community.

去年， Tsaatan 人知道蒙古政府计划花150万美元开发他们的社区。

Institute for Mongolian, Buddhist and Tibetan Studies of the Siberian Division of the Russian Academy of Sciences, Russia）: Latinization of Buryat-Mongolian Script: An Experience of Language Unification in a Polyethnic Society

巴扎若夫、V.V(俄罗斯科学院西伯利亚分院蒙藏佛教研究中心，俄罗斯)：布利亚特蒙古文字的拉丁化-多民族社会的语言同意实践

1:250000 geological mapping has further revealed the mysteries of the tectonics of the Qinghai-Tibet Plateau. The Altun Mountains are not of the Tarim massif, but a part of the Kunlun-Qilian-Qinling orogenic system; the Altun fault is a large transform fault; the Muztag-Maqên suture zone and Jinshajiang suture zone are both Variscan ones; the Songpan-Garzê area in the Triassic was a huge turbidite basin on the southern margin of Laurasia; the Gangdise belt underwent the important Indosinian orogenic movement; an ocean basin that persisted from the Paleozoic to Triassic did not exist, i.e. the so-called Paleo-Tethys or permanent Tethys was not in existence in the Qinghai-Tibet Plateau. In the Paleozoic, most parts of China, including the Sino-Korean, Yangtze and Tarim massifs and the Qinghai-Tibet Plateau, were located in south of the main ocean basin—the Central Asian-Mongolian sea way—of the Paleo-Asia ocean, belonging to the northern margin of Gondwana. The Yarlung Zangbo and Bangong -Nujiang belts were twins in the Tethyan Ocean, which began to develop into two ocean rift belts in the Triassic. The Tethyan Ocean with the Yarlung Zangbo belt as the main ocean basin belt began to be subducted in the Late Triassic and experienced a process of pulsatory plate convergence orogeny including the Indosinian, Yanshanian and Himalayan stages.

1：25万地质填图进一步揭开了青藏高原地区大地构造的奥秘：阿尔金山是昆仑，祁连-秦岭造山系的一部分；阿尔金断裂确是一条大型转换断层；木孜塔格-玛沁缝合带和金沙江缝合带均是华力西缝合带；松潘甘孜三叠系沉积盆地是劳亚大陆南部边缘的浊积岩盆地；冈底斯带曾经历了重要的印支造山运动；不存在从古生代延续到三叠纪的大洋盆地，即不存在所谓古特提斯或永久特提斯；古生代时期，在青藏高原地区亦不存在具古生物，古地理分隔意义的大洋盆地，当时，包括中朝，扬子，塔里木以及青藏高原地区在内的中国大部分均位于古亚洲洋主洋盆——中亚-蒙古带之南，属冈瓦纳大陆结构复杂的北部边缘；雅鲁藏布江和班公湖-怒江带是特提斯洋中的孪生姊妹，它们均是从三叠纪起就发展成大洋裂谷带的；以雅鲁藏布江带为主洋盆带的特提斯洋，从三叠纪晚期开始消减，经历了印支，燕山，喜马拉雅3个阶段脉动式板块汇聚造山过程。

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。