柴达木盆地东南部,southeastern Caidamu basin
1)southeastern Caidamu basin柴达木盆地东南部
1.Hereby,the evaluation insoutheastern Caidamu basin focuses on discussing the land resources,to be exact,to classify the land resources,which is,on the point of degeneration,to grade its types in the such environment.柴达木盆地东南部地区风沙环境评价重点是对土地资源的评价。
英文短句/例句
1.Study on Sphecia siningensis Difference between South-east Chaidamu Basin and Yulin Shanxi柴达木盆地东南部杨干透翅蛾与陕西榆林的差异研究
2.PALEOCLIMATE EVOLUTION IN SOUTHEAST OF QAIDAM BASIN SINCE THE LAST INTERGLACIAL浅析末次间冰期以来柴达木盆地东南部古气候环境演化
3.Study on Thermochronology of Southeastern Qaidam Basin and Its Tectonic Implications, Qinghai Province, NW China;柴达木盆地东南缘热年代学与构造演化
4.Geochemical Characteristics and Classification of Natural Gas in Quaternary in the East Part of Chaidamu Basin柴达木盆地东部第四系天然气地化特征与分类
5.Zeolite Distribution Characteristics and Contributing Factors in Southern Region of West Qaidam Basin柴达木盆地西部南区沸石分布特征及成因
6.Formation of Gas Reservoirs in Quaternary at the East Part of ChaidamuBasin and Their Exploration Prospects柴达木盆地东部第四系气藏的形成和勘探前景
7.Environmental Changes and Cultural Transition at Late Holocene in Qaidam Basin;柴达木盆地东部环境演化对古文化的影响
8.The Preliminary Study on Mesozoic Hydrocarbon Character in the Eastern Part of Qaidam Basin柴达木盆地东部中生界含油气性初步研究
9.Changes in Eastern Asian Winter Monsoon Recorded by Aeolion Deposits at the Southeastern Margin of Qaidam Basin Over the Past 5000 Years近5000a来柴达木盆地东南缘风成沉积记录的冬季风演化
10.Discussion on the Control of E_3~1 Sedimentary Facies over Sandbody Distribution of Gas Slap Southeast Area in Qaidam Basin柴达木盆地尕斯东南斜坡E_3~1沉积相对砂体分布的控制探讨
11.Geochemical Research in LC 1 Well of Tertiary Source Rocks in the South Area of Western Qaidam Basin柴达木盆地西部南区绿参1井烃源岩地球化学研究
12.DISTRIBUTION LAWS AND EVALUATION OF HYDROCARBON POTENTIAL ON CARBONIFEROUS IN THE EAST OF QAIDAM BASIN柴达木盆地东部地区石炭系分布规律与生烃潜力评价
13.GEOCHEMICAL PROPERTIES OF SOURCE MATERIALS AND BIOGAS PROSPECTS OF THE QUATERNARY GAS IN EAST OF QAIDAM BASIN柴达木盆地东部第四系气源岩地化特征与生物气前景
14.Evaluation of Circulareconomy Development in Eastern Area of Chaidamu Basin Based on AHP Data Analysis;基于AHP分析的柴达木盆地东部地区循环经济发展评价
15.Geochemical characteristics and play targets of gas in eastern Qaidam Basin,NW China柴达木盆地东部天然气地球化学特征与勘探方向
16.Distribution Rules of Hydrocarbon in the Cenozoic Erathem of Western Qaidam Basin柴达木盆地西部新生界油气分布规律
17.Cenozoic structurestyle and dynamics significance in southwestern Qadam Basin柴达木盆地西南部新生代构造样式及其动力学特征
18.A study on sedimentary facies of the Neogene and exploration prospective of sandstone-type uranium deposits in eastern Chaidam Basin柴达木盆地东部新近系沉积相与砂岩型铀矿找矿方向
相关短句/例句
eastern Qaidam Basin柴达木盆地东部
1.Geophysical response of unconformities and petroleum geological significance in theeastern Qaidam Basin;柴达木盆地东部不整合结构的地球物理响应及油气地质意义
2.Evaluation of Carboniferous hydrocarbon source rocks in the eastern Qaidam basin,China;柴达木盆地东部石炭系烃源岩评价
3.Relationship between unconformity and hydrocarbon accumulation in the Mesozoic ofeastern Qaidam Basin;柴达木盆地东部地区中生界不整合与油气成藏的关系
3)Southeastern Qaidam柴达木盆地东南缘
1.Study on Thermochronology ofSoutheastern Qaidam Basin and Its Tectonic Implications, Qinghai Province, NW China;柴达木盆地东南缘热年代学与构造演化
4)the northeast part of the Qaidam Basin柴达木盆地东北部
5)Middle-East area of Qaidam Basin柴达木盆地中东部
6)central south Qaidam basin柴达木盆地中南部
1.Petroleum geology conditions and exploration perspective incentral south Qaidam basin;柴达木盆地中南部第三系石油地质条件与勘探前景
延伸阅读
柴达木盆地自然资源柴达木盆地自然资源natural resources of Chaidamu basinehaidamu Pend一ziran ziyuan柴达木盆地自然资源(natural~二es of Chaldamu1)asin)柴达木盆地位于青藏高原北部，青海省西北部。面积约25万平方千米，盆地最低处海拔261)~28(X)米，为中国最高的封闭式内陆盆地。“柴达木”在蒙古语中是“盐泽”之意。盆地内大于1平方千米的天然湖泊42个，面积1%7平方千米，其中咸水湖、盐湖27个。柴达木盆地矿产资源丰富，盐湖资源得天独厚。目前，已探明储量的矿种50余种，矿点208处，盐湖20余个，湖盐储量以刀多亿吨。其中，氯化钾、氯化铿、氯化镁、澳、池盐、惚矿、黄金、芒硝、天青石化工用石灰岩、石棉均居全国首位;三氧化二硼与氯化铆、碘、天然碱居全国第二位和第三位。钾盐是中国的短缺矿种，察尔汗盐湖是中国最大的钾镁盐基地。它包括别勒滩、达尔逊、察尔汗和霍布逊等盐湖、盐滩，面积5856平方千米，被称为“银海盐原”。青藏公路途经此地有一段32千米长的盐晶公路被称为“万丈盐桥”。其他盐类矿产地还有大浪滩钾镁盐矿、大小柴旦盐湖硼矿、一里坪、东西台吉乃尔铿盐矿、茶卡、柯柯池盐矿等。这些盐矿储量丰富且多矿种伴生。锡铁山是中国重要的铅锌矿产地，以铅锌矿为主，伴生有金、银、锡、锑、铜、砷、锅、锢、稼等稀有金属矿产。其中铅品位3.73%，锌4.23%，金0.59克/吨，银42克/吨。铁矿分布在格尔木以西的肯德可克和都兰县，以矽长磁铁矿为主。盆地西端的茫崖有蛇纹石石棉，含棉率为5%~25%，纤维长度1~3毫米。柴达木盆地是中国ro大沉积盆地之一，具有丰富的能源矿产。煤系地层为石炭系及侏罗系，分布在柴北与昆仑山前两大部分。其中，以鱼卡至耗牛山一带比较集中。现已查明两个生油层，一个含气层，发现油田16个，气田6个。另外，在6个构造上有工业油流，40个构造中有油气显示，探明石油地质储量1.88亿吨，天然气472亿立方米。油田主要分布在盆地西北部，有冷湖油田、尖顶山油田、花土沟油田和孕斯库勒油田。天然气分布在盆地中部东西台吉乃尔湖和涩聂湖地区，有涩北气田、盐湖气田等。柴达木盆地的土地资源潜力也很大，现有宜垦荒地2(X)余万亩，可利用草场593多万公顷，柴达木盆地是一个“聚宝盆”，在20世纪末、21世纪初，随着国家开发建设重点的转移，它将是中国经济开拓的重点地区。(李容全)
