喜马拉雅

Eastern Himalaya Syntaxis is an important area in studying climatic-tectonic reciprocity. In this paper, single-crystal-high-precision laser ~(40)Ar/~(39)Ar method was used to build the thermal evolutional history of Eastern Himalaya Syntaxis by tests on river sediments on the lower reach of Yalung-Tsangpo River. The contrast of age statistical results against the figure showing the changes in rate and angle of convergence during India plate has been colliding against Eurasian plate since late Mesozoic and the diagram consisting of global deep-seaδ18O andδ13C records is done, for the purpose of revealing climatic and tectonic information on rock cooling and referring the relationship between thermal evolutional history and climate and tectonics.

东喜马拉雅构造结是气候与构造相互作用的典型地区，本文尝试使用单颗粒高精度单次全熔~(40)Ar/~(39)Ar法对采自雅鲁藏布江大峡谷下游墨脱县城以南约50 km处地东河段的细粒现代河沙进行年代学测试，建立东喜马拉雅构造结的热史演化序列，并通过与代表全球气候变化的18O、13C浓度变化曲线和印度大陆向北运动的速度、角度变化曲线的对比，揭示气候、构造因素与东喜马拉雅构造结热史演化的耦合，推定热史演化与气候、构造过程的关系。

The contrast of age statistical results against the figure showing the changes in rate and angle of convergence during India plate has been colliding against Eurasian plate since late Mesozoic and the diagram consisting of global deep-seaδ18O andδ13C records is done, for the purpose of revealing climatic and tectonic information on rock cooling and referring the relationship between thermal evolutional history and climate and tectonics.

东喜马拉雅构造结是气候与构造相互作用的典型地区，本文尝试使用单颗粒高精度单次全熔40Ar/39Ar法对采自雅鲁藏布江大峡谷下游墨脱县城以南约50 km处地东河段的细粒现代河沙进行年代学测试，建立东喜马拉雅构造结的热史演化序列，并通过与代表全球气候变化的18O、13C浓度变化曲线和印度大陆向北运动的速度、角度变化曲线的对比，揭示气候、构造因素与东喜马拉雅构造结热史演化的耦合，推定热史演化与气候、构造过程的关系。

Marmota himalayana, Microtus oeconomus, Mus musculus, Cricetulus longicaudatus, Ochotona curzoniae, Felis catus, Canis familiaris, Vulpes vulpes, Vulpes corsac, Canis upus, Mustela eversmanni distributed widely in Sanjiangyuan Area.

三江源地区喜马拉雅旱獭、根田鼠、小家鼠、长尾仓鼠、高原鼠兔、猫、犬、赤狐、沙狐、狼、艾鼬等广泛分布，其中喜马拉雅旱獭是青藏高原喜马拉雅旱獭鼠疫自然疫源地的主要宿主。

Studies of the evolution and changes in the Tethys Ocean occurring during past 200 Ma may provide a model for fut...

在对藏南白垩纪沉积地质详细研究基础上，本文对尼泊尔喜马拉雅和Lhadkh喜马拉雅白垩系进行了对比。

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。

Truth is, the Himalayas are between you two, and China's never coming over the Himalayas.

事实是：喜马拉雅山就在你们中间，而中国是从不翻越喜马拉雅山的。

There has been too much focus on glaciers whereas there are other factors like precipitation and snowfall that affect the levels of waters in rivers downstream the eastern Himalayas, says Mats Eriksson , a senior hydrologist with the Nepal-based International Centre for Integrated Mountain Development, which has carried out several studies on the glaciers in the Hindu Kush Himalayas.

尼泊尔国际山地综合发展中心的高级水文学家麦茨。埃里克森认为，人们给冰川的关注太多，忽略了其他因素也可能影响发源于东喜马拉雅山的河流流量，比如降水和降雪等。ICIDOD最近对印度库什喜马拉雅山冰川展开了研究。

In central Himalaya, massif was mainly uplifted in the tectonic model of channel flow during 17~7 Ma at a velocity of ~2 mm/a, then was extruded to earth surface at a much lower velocity. In eastern Himalaya Syntaxis, massif was mainly uplifted in the structural style of titling at a background of isostasy since 4.0~2.2 Ma.

喜马拉雅中段主要在17~7 Ma前以通道流的方式快速隆升，之后的抬升过程相对缓慢；东喜马拉雅构造结则主要在3 Ma以来，以地壳均衡作用为背景的掀斜式抬升为主要隆升模式。

According to the three-components teleseismic records from portable digital seismic station deployed in Himalaya mountain chain region, the S-wave velocity structure beneath 46 teleseismic stations are investigated by using transform function method and SA technique. As reliable geophysics evidence, these results help us to understand the geodynamic process of Himalaya mountain region of Tibet.

利用流动数字地震台网提供的三分量地震波形记录，应用转换函数及快速模拟退火算法对喜马拉雅山脉地区46个地震站下的地壳横波速度结构进行了反演，为进一步揭示青藏高原喜马拉雅山脉地区的动力学演化过程提供了可靠的地球物理证据。

In this paper, four sections located respectively in Yadong-ZhergerLa in central Himalaya, Pai-Zaqu reach of Yalung-Tsangpo River, west slope section of NamuLa and east slope section of DuoxiongLa in Eastern Himalaya Syntaxis were chosen, and conventional and laser ~(40)Ar/~(39)Ar methods were used to build the framework of thermal evolution history of central-east part of Himalaya orogen, for the purpose of revealing the secret of uplif of central-east Himalaya.In Yadong district in central Himalaya, a retro-metamorphic high-pressure granulite and its country rock were focused and conventional ~(40)Ar/~(39)Ar tests were done.

本文选择位于喜马拉雅中段亚东地区的亚东—哲古拉剖面以及位于东喜马拉雅构造结的雅鲁藏布江沿岸派乡—扎曲段、那木拉峰西坡以及多雄拉峰东坡等四条剖面，利用精细的阶步加温和单次全熔~(40)Ar/~(39)Ar年代学方法，试图构建喜马拉雅中段及东喜马拉雅构造结岩体热史演化的年代学框架，以期解开喜马拉雅造山带中东段的抬升之谜。

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。