吐鲁番-哈密盆地,Turpan-Hami basin
1)Turpan-Hami basin吐鲁番-哈密盆地
1.Lies in the eastern Xinjiang,the Turpan-Hami Basin is one of the three most important large oil-enriched basins in Xinjiang district.吐鲁番-哈密盆地位于新疆东部,是新疆三大油气盆地之一。
英文短句/例句

1.LATE EARLY PERMIAN ANGARA FLORA FROM TURPAN-HAMI BASIN吐鲁番-哈密盆地早二叠世晚期植物群
2.HYDROCARBON PROSPECTS OF CENOZOIC SYSTEM IN TURPAN-HAMI BASIN FROM VIEW OF ORGANIC MATTER EVOLUTION从有机质的演变程度展望吐鲁番-哈密盆地中生界油气前景
3.FORMATION,EVOLUTION OF TURPAN-HAMI BASIN AND ITS PETROLIFEROUS PROSPECTIVE EVALUATION吐鲁番—哈密盆地形成演化与含油气远景评价
4.Early-Middle Jurassic Stratigraphy and Palynological Assemblages of the Taibei Depression in the Turpan-Hami Basin吐鲁番—哈密盆地台北凹陷早、中侏罗世地层及孢粉组合研究
5.However, Taoism was limited mainly to the Turpan and Hami areas, where Han people were concentrated.但是传播范围不广,主要盛行于汉人比较集中的吐鲁番、哈密等地。
6.Spatial and Temporal Characteristics of Sand-dust in Turpan Basin in Recent 30 Years吐鲁番盆地近30年沙尘天气分布特征
7.The Turpan Basin in Xinjiang is the world's lowest-lying basin.中国新疆的吐鲁番盆地是世界最低的盆地。
8.Soil Temperature Change Characteristics in Energy-Saving Heliogreenhouse and Its Application in Turpan Basin吐鲁番盆地节能日光温室地温变化特征及应用
9.THE UTILIZATION OF WATER RESOURCES AND THE OASIS ECONOMIC DEVELOPMENT IN TURPAN BASIN吐鲁番盆地水资源利用与绿洲经济发展探讨
10.OBSERVATION ON THE BIONOMICS OF PHLEBOTOMUS ALEXANDRI IN TURFAN BASIN, XINJIANG新疆吐鲁番盆地亚历山大白蛉生态的调查研究
11.Initial Explore for the Groundwater Resources’ Development and Utilization and Protection Measures of Turpan Basin吐鲁番盆地地下水资源开发利用及保护对策初探
12.The Turban Basin in Xinjiang is the world's lowest-lying basin, the lowest point being 154 metres below sea level.中国新疆的吐鲁番盆地是世界最低的盆地。 盆地最低点在海平面以下154米。
13.In striking contrast to the cool world of the mountain and the lake is that furnace of a place, the Turpan Basin.与清凉世界--天池形成强烈反差的是“火州”--吐鲁番盆地。
14.The Annual Extreme Value Distributing Analysis on Turpan s Day Maximum Precipitation in Its Basin and Plain and Mountain Areas;浅析吐鲁番盆地平原及山区一日最大降水量年极值的分布
15.The Elementary Analysis about Water Resources of Turpan Basin and Oasis and Agriculture Development;吐鲁番盆地水资源与绿洲及农业可持续发展初步分析
16.Discussion on the Water Resources and Their Rational Development and Utilization in Turpan Basin吐鲁番盆地的水资源运转规律及其持续利用研究
17.Fluid geochemistry, dynamics and hydrocarbon migration and accumulation in Lukeqin structure, Turpan Hami basin吐哈盆地鲁克沁构造带流体地球化学、动力与油气运移和聚集
18.The heavy oil reservoirs of Lukeqin structure belt are in distribution areas of pre-Jurassic heavy oil reservoirs which is discovered in the Turpan-Hami basin.鲁克沁构造带稠油藏属于吐哈盆地前侏罗系稠油分布区。
相关短句/例句

Turpan Hami Basin吐鲁番-哈密盆地
1.The Upper Permian, Triassic and Jurassic strata in the Turpan Hami basin have a wide distribution of alluvial fan, fluviolacustrine deposit, fan delta, braided delta and normal delta deposit, which are most characterized by the fan delta and braided delta deposits whose skeletons are mainly channel sandbodies.吐鲁番-哈密盆地上二叠统、三叠系和侏罗系广泛发育冲积扇、河流、湖泊、扇三角洲、辫状河三角洲和正常三角洲相沉积。
3)Tulufan-Hami Basin吐鲁番-哈密盆地
1.Based on the theory of sequence stratigraphy,the sequence features of the Jurassic at the southern margin of Tulufan-Hami Basin have been analyzed and three type of I sequences have been identificated approximately corresponding to Badaowan,Sangonghe and Xishanyao Formations respectively.本文运用层序地层学理论和工作方法,对吐鲁番-哈密盆地南缘诛罗系地层进行了详细研究,识别出3个I类层序,分别与岩石地层单位八道湾组、三工河组、西山窑组大致相当;在层序体系域、沉积体系研究的基础上,指出层序内高水位体系域(HST)中的辫状河三角洲体系是层间氧化带砂岩型铀矿产出的有利层位。
4)Tulufan basin吐鲁番盆地
1.Coordination of Rapid Developing of Economy and Exploiting of Water Resources——Illustrated by That of Hangjiahu Plain and Tulufan Basin;协调好高速发展经济和开发利用水资源的关系——以杭嘉湖平原和吐鲁番盆地为例
5)Turpan basin吐鲁番盆地
1.The Elementary Analysis about Water Resources of Turpan Basin and Oasis and Agriculture Development;吐鲁番盆地水资源与绿洲及农业可持续发展初步分析
2.Environmental Proxies from the Terrestrial Cretaceous-Paleogene Boundary in the Turpan Basin,Xinjiang;新疆吐鲁番盆地陆相白垩纪与古近纪界线的环境指标
3.Quaternary climate change in Turpan basin and its significance to sandstone-type uranium mineralization;吐鲁番盆地第四纪气候变迁及其对砂岩型铀成矿作用的意义
6)Junggar southern margin-Turpan准噶尔南缘-吐鲁番盆地
延伸阅读

吐鲁番盆地吐鲁番盆地位于中国新疆维吾尔自治区东部。是博格达山和觉罗塔格间的陷落盆地。东西长200千米,南北宽80千米。面积3470平方千米。地势北高南低,中部的艾丁湖(觉洛浣)水面低于海面154米。为中国陆上最低点。是中国夏季最炎热地区,气温最高曾达48.9℃,40℃以上日数30多天,地面温度82.3℃,是沙煮蛋、石烙饼的地方,古有火洲之称。1961~1970年年均降水量3.9毫米,蒸发量3000毫米以上。风力强劲,夏季热风,吹枯作物。戈壁滩、沙漠发育。属荒漠地形,呈环状结构。盆地四周是一圈戈壁砾石带,高山冰川雪水流向盆地低处,在山前形成地下水库;东部有小片沙漠称库姆塔格(即沙山),沙丘不移动;北部火焰山前缘为泥沙旱三角洲,赖坎儿井灌溉,发展农业。全区共有坎儿井1100多条,井长3~30千米,灌溉70%的田地。盛产棉花、葡萄、哈密瓜。