查询词典 Kunlun

Tibet has very complex topography and falls into three geographic parts: the northern part of Tibet known as the North-Tibet Plateau, lies between Kunlun Mountain, Tonglha Mountain and Kangdese Mountain, and Nyainqentanglha Mountain;between Kangdese Mountains and Himalayas;the river valleys which the the Yarlung Tsangpo and its anabranch flow by in the southern part of Tibet and lie between the Gangdise and the Himalaya ranges; the eastern part of Tibet belongs to an area of deep gorges where a series of mountain ranges from east to west criss-crossing mountain ranges running from south to north,and is some parts of the Hengduan mountain range.

在西藏的边远山谷中，一辆老式的苏联卡车翻滚到坡底的河边，车里一个已经怀孕了几个月的女人尽然不死，而她腹中的孩子也没死，那个孩子尽然就是我。"——莫毅，这为神交已久而未谋面的艺术家，其作品在许多展览上令我印象深刻，在筹备此展的过程中认识，相聊甚欢。多年藏区生活塑造了一个率直敏锐的性情汉子，这组拍摄于20年前、却完成于今年的作品以严肃的记实性和抒情的叙事片段，融会艺术家近年的实验手段，呈现了对诸如"脆弱"、"意外"、"真实"和"理想"的记忆。因此20年后的莫毅仍然"想念西藏。

By the budgetary estimate of the water and heat conditions at the glacial equilibrium line and the water balance of lakes in the area of the West Kunlun Mountains during the late stadial of the Last Glaciation. before the summer mean temperature decreased by 1.5 C, the annal mean precipitation was 10-20% more than that of the present. As the summer mean temperature lowering was over 1. 5 C, the precipitation was decreased and the negtive of the lake water balance appeared.

文中还根据对西昆仑山区冰川零平衡线处水热状况及湖泊水量平衡状况的推算，指出末次盛冰期中，在夏季温度降低1-1.5℃以前，其年降水量应大于现代值，增加量大约在10-20％左右；在夏季温度降低值大于1-1.5℃以后，其降水减少，湖泊水量平衡出现负值，这与冰川、湖泊变化的地质记录所反映的早期冷湿、中期冷干气候条件相符。

As an attempt, we inverse the assumingly active faults' slips triggered by the M8.1 Kunlun Mountain earthquake over Beijing area.

作为尝试，对昆仑山口西M8.1地震触发的北京地区断层活动进行了反演。

Its impact on"A Chinese Bestiary"and"Songs of Chu"represented by Qu Fu profoundly developed to a kind of complex—Kunlun complex—in the two books.

不仅如此，《山海经》和屈赋还都在原始宗教——巫风的背景下生成、发展，其中记载的很多神话都可以。。。

Based on surface and subsurface geological data, combined with achievements about the west Kunlun orogen, Tibet, Tarim basin and Altun tectonic zone, it is analysed that geometry and kinematics of the west Kunlun fold-thrust-belt between Sangzhu country in the west and Cele county in the east.

本文通过对研究区地面地质资料和地下地质资料的分析，并结合西昆仑造山带、青藏高原、塔里木盆地和阿尔金构造带研究的新进展，对西昆仑北缘冲断带桑株—策勒段的构造形态和演化历史作了深入的剖析与探讨，取得了一些新认识。

Based on the settings and geological and geochemical characteristics of granitoids of different orogenic belts (exemplified by orogenic granitoids in Altay, East Kunlun, Yanshan in North China, Northeast China and Nanling in South China), the relationships between granitoids and continental crustal growth are discussed, and five modes of continental crustal growth in the continent of China are proposed;they are as follows:(1)the Altay mode of continental growth is that the material and heat of the Paleozoic convertive mantle formed on the background of the Paleo-Asian Ocean were input into the Paleozoic continent and mixed with the materials of the upper crust;(2) the East Kunlun mode is that the basement of the Proterozoic orogenic belt was reworked by the heat input and materials of the Paleozoic-early Mesozoic convective mantle formed on the background of TTG continental crust of the Proterozoic orogenic belt;(3) the Northeast China style is that the Phanerozoic continental crust was reworked by the heat input and materials from the convective mantle formed on the background of the Yanshanian Central Asian orogenic belt;(4) the Yanshan mode is that the Archean basement was reworked by the heat input and materials from the Yanshanian convective mantle;and (5) the Nanling mode is that in South China what was input by the Yanshanian convective mantle into the continent was mainly heat and subordinately materials and the crustal material recycle was the dominant mode for the continental growth (showing zero continental growth).

根据不同造山带花岗岩的形成背景，地质地球化学特征差异，以阿尔泰，东昆仑，华北燕山，东北和南岭造山带花岗岩为例讨论花岗岩与大陆地壳生长的关系，区分出中国大陆的5种大陆地壳生长方式：阿尔泰式是古亚洲洋背景上形成的古生代对流地幔物质，热输入和上地壳混合为主的方式；东昆仑式是元古代造山带TTG陆壳背景基础上古生代—早中生代对流地幔物质和热输入，改造元古宙造山带基底的方式；东北式是燕山期中亚造山带背景上对流地幔物质和热输入改造显生宙陆壳的生长方式；燕山式是燕山期对流地幔物质和热输入改造太古宙基底的方式；南岭式燕山期对流地幔输入大陆的是以热为主，物质为辅，大陆地壳生长是以陆壳物质再循环为主的生长方式。

Paleomagnetic study shows that the molasse in the front of the West Kunlun formed in the late Miocene to early-mid Pliocene,reflecting that a rapid uplift process took place in the West Kunlun-Qinghai-Tibet Plateau in the late Miocene.

古地磁研究结果显示，西昆仑山前磨拉石形成于中新世晚期一上新世早中期，反映西昆仑山一青藏高原在中新世晚期有一次快速的隆升过程。

Brief Introduction: Mount Muztag lies on the west of the Kunlun Mountains, 75.1°E, 38.5°N. It is the second highest peak of the Kunlun Mountains. Occupying an area of 258 square kilometers and with fault scarps and a relatively smooth top surface, this block mountain developed modern glaciers, the endsof which reach heights from 5020 to 3900 meters. The largest two, the Xili and Kematule Gllaciers, split the mountain body into half transversely. Slopes on west face of the mountain are even, whereas those on north and east faces are quite rugged.

简要说明：慕士塔格峰位于西昆仑山，为昆仑山第二高峰（海拔7509米），位于东经75.1度，北纬38.5度，为有断崖发育的断块山地，顶面较平，现代冰川发育，面积达258平方公里，冰川末端海拔3900～5020米，其中最大的栖力冰川和克麻土勒冰川将山体横切为两半，山峰西边坡势平缓，北边和东边却十分险峻。

But now the kunlun mountains is the kunlun mountains in history?

而现在的昆仑是不是就是历史上的昆仑呢？

Although the kunlun mountains, but not sure position in zhongyuan northwest kunlun about is without a doubt.

尽管昆仑山的位置没有确定，但昆仑山在中原西北方大约是没有疑问的。

Fancy gold-plated dangling earrings with facetted White Opal crystals.

花式镀金悬垂耳环与facetted白欧泊水晶。

This essay chooses the study aim from biology teachers in middle school in Shi Jiazhuang which tells us that most of the middle school biology teachers in Shi Jiazhuang have the"burnout", lower successfulness, individualize.

本文选取石家庄市初中生物教师作为研究对象，运用问卷调查的方法对石家庄市初中生物教师职业倦怠的现状进行调查，调查结果发现，石家庄市初中生物教师这一群体普遍存在职业倦怠，情感枯竭程度偏高，成就感偏低，去个性化程度最为严重。