塔里木盆地,Tarim Basin
1)Tarim Basin塔里木盆地
1.Reservoir accumulation pattern of multi-factor recombination and procession superimposition and its application inTarim Basin;塔里木盆地“多元复合—过程叠加”成藏模式及其应用
2.Aromatic Compositions of Different Occurrence States in Deep Carbonate Rocks fromTarim Basin;塔里木盆地深层碳酸盐岩中不同赋存形式芳烃化合物组成
3.Upper Cambrian-Ordovician reservoir characteristics in Well Gucheng-4 area,Tarim Basin;塔里木盆地古城4井区上寒武统—奥陶系储集层特征
英文短句/例句
1.The Basin-Range Coupling and Hydrocarbon Accumulation in the East Tarim Basin塔里木盆地东部盆山耦合与油气成藏
parison of Geological Characteristics Between the Caspian Basin and the Tarim Basin滨里海盆地与塔里木盆地油气地质特征的类比
3.Petroleum Geologic Features of Cambrian-Ordovician in Tarim Basin塔里木盆地寒武──奥陶系石油地质特征
4.STUDY ON SEQUENCE STRATIGRAPHY OF ORDOVICIAN IN NORTH TARIM BASIN塔里木盆地北部奥陶系层序地层研究
5.THE PALEOZOIC SEQUENCE STRATIGRAPHIC SYSTEM IN NORTHERN TARIM BASIN塔里木盆地北部古生代层序地层系统
6.Study on Some Species of Ascochyta Collected from Desert Region of Tarim Basin(Ⅰ)塔里木盆地荒漠地区壳二孢研究(Ⅰ)
7.Sequence Stratigraphy Study of Silurian in Tazhong Area, Tarim Basin;塔里木盆地塔中地区志留系层序地层学研究
8.Study on Basin-Range Coupling & Petroleum Accumulation in the East Region of Tarim Basin;塔里木盆地东部地区盆山耦合与油气聚集
9.Sequence Stratigraphy of upper Devonian-Carboniferous in Tarim Basin塔里木盆地上泥盆统—石炭系层序地层学研究
10.IDENTIFICATION AND PREDICTION OF VOLCANIC BODIES IN TAZHONG AREA OF THE TARIM BASIN塔里木盆地塔中地区火成岩体识别与预测技术
11.Study on the Petroleum Accumulation System Within the Tazhong Region, Tarim Basin;塔里木盆地塔中地区油气成藏体系研究
12.Analysis of Fractured Reservoirs in Ordovician in Tazhong Area, Tarim Basin;塔里木盆地塔中地区奥陶系裂缝储层发育特征
13.The Structural Characteristics Research and Structural Zones Evaluation of Ta Dong Area in Tarim Basin;塔里木盆地塔东地区构造特征研究与区带评价
14.Diapir structure and its relationship with petroleum accumulation in Tazhong area,Tarim Basin塔里木盆地塔中地区底辟构造与油气关系
15.The mountain barrier to the west of this Tarim Basin is high.塔里木盆地西边的山障是很高的。
16.Study on the Characteristic of Sedimentology and Hydrocarbon Accumulation in Eastern Tarim Basin塔里木盆地东部沉积及成藏特征研究
17.The Research of Pool-forming Mechanism of Hadexun Oilfield in Tarim Basin;塔里木盆地哈得逊油田成藏机理研究
18.The Study on Velocity Field of Bachu Uplift in the East Part of Tarim Basin;塔里木盆地巴楚隆起东段速度场研究
相关短句/例句
the Tarim Basin塔里木盆地
1.Depositional feature of Permian system in Tazhong area ofthe Tarim Basin;塔里木盆地塔中地区二叠系沉积特征
2.Oil sources analyses of Mesozoic group reservoirs in Lunnan area ofthe Tarim Basin.;塔里木盆地轮南地区中生界油藏油源分析
3.A relation of Between the Prosperity and Decline of Loulan andthe Tarim Basin Environment Evolved;楼兰城的兴衰与塔里木盆地环境演变之间的关系
3)Talimu Basin塔里木盆地
1.Gas source analysis of Yingnan-2 gas reservoir in the eastern part ofTalimu Basin;塔里木盆地塔东英南2气藏气源分析
2.Discussion on oil reservoir forming conditions and exploration targets of the Silurian inTalimu Basin;塔里木盆地志留系成藏条件与勘探方向探讨
3.Experimental study of the oil and gas migration and accumulation process of Wushi Sag-Wensu Uplift inTalimu Basin;塔里木盆地乌什凹陷—温宿凸起油气运聚过程模拟实验研究
4)Tarim塔里木盆地
1.Understandings and solutions of increasing drilling speed inTarim basin;提高塔里木盆地钻井速度的认识与对策
2.The Carbonate Depositional Features of Yigeziya Formation of Upper CretaceousinTarim Basin and Their Geological Implication;塔里木盆地上白垩统依格孜牙组碳酸盐岩沉积学特征及地质意义
3.New Advances in the Study of the Devonian-CarboniferousBoundary in theTarim Basin;塔里木盆地泥盆系-石炭系界线研究新进展
5)Ordovician[英][,?:d?"vi??n][美][,?rd?"v???n]塔里木盆地
1.Genesis Classification and Characteristics ofOrdovician Carbonate Reservoirs and Petroleum Exploration Potential in Tazhong Region,Tarim Basin;塔里木盆地塔中地区奥陶系碳酸盐岩储层成因类型、特征及油气勘探潜力
2.The Small Scale Sequence Stratigraphy of TheOrdovician Carbonate of the Sangtamu Horst in The Tarim Basin;小尺度的碳酸盐岩层序地层学分析——塔里木盆地桑塔木断垒带奥陶系层序地层学研究
3.Cases of Discovery and Exploration of Marine Fields in China (Part 12):LunnanOrdovician Oil-Gas Field in Tarim Basin中国海相油气田勘探实例之十二塔里木盆地轮南奥陶系油气田的勘探与发现
6)center of the Tarim basin塔里木盆地腹地
延伸阅读
塔里木盆地塔里木盆地中国第一大内陆盆地。位于新疆维吾尔自治区南部。西起帕米尔高原东麓，东到罗布泊洼地，北至天山山脉南麓，南至昆仑山脉北麓，大致在北纬37°～42°的暖温带范围内。盆地东西长1400千米，南北宽约550千米。面积约53万平方千米。四周高山海拔4000～6000米，盆地中部海拔800～1300米，地势由南向北缓斜并由西向东稍倾。边界受东西向和北西向深大断裂控制，成为不规则的菱形，并在东部以70千米宽的通道与河西走廊相接。居亚洲大陆中心，气候干燥，雨量特少，如若羌1957年全年降水量3.9毫米，民丰安迪尔1966年降水量5.0毫米，蒸发量却很大，若羌达2952毫米，故以风力作用为主，风速常在5米/秒以上，石蘑菇和风城地貌发育。自然景色分成4个环状：①盆地边缘砾石带棗山足戈壁滩，是由古代暴流洪积扇群组成，微向盆地中心倾斜，坡度一般6°～8°，宽度10～30千米，厚度千米以上，表面由2～3米厚砾层组成，水均渗入地下，地面草木不生。②盆地边缘绿洲带，河流出山之后，坡度突降，水流分散，沙泥沉积，形成扇状平原，现有疏勒、莎车、阿克苏、和田和库车等大小绿洲100多个。绿洲灌溉农业发达，盛产小麦、玉米、水稻和棉花等，河道迁移，绿洲也会迁移。③盆地中部沙漠带，即塔克拉玛干沙漠，面积32.4万平方千米，占中国沙漠面积的47％，为世界上第二大沙漠。主要是流动沙丘，占85％，沙丘高大，多50米以上，成沙较老的可达250米，呈新月形沙丘、新月形沙丘链，复合型沙山、长条状沙丘、金字塔形沙丘等形态。④盆地东部的罗布泊湖盆区，大部由盐壳组成，范围曾有多次变动，多风蚀雅丹地形。塔里木河基本汇集了盆地的全部大河，全长2000千米，为中国最长的内陆河。河流冲积平原土地资源丰富，胡杨林和灰杨林分布面积广，对防御风沙、调节气候、供应木材有重要作用。塔里木盆地中的巴楚烽火台
