柴达木盆地太阳能光辐站
柴达木盆地位于青海省北部。
The Chaidamu Basin is situated in the north part of Qinghai Province.
柴达木盆地是中国陆上第四大天然气产区。
The Qaidam Basin is the fourth large natural gas production area.
目的分析柴达木盆地第三纪盐湖的沉积环境。
Aim To analyze Tertiary period sedimentary environment of Qaidamu saline lake.
最宽处在酒泉与柴达木盆地之间，达300公里。
Widest point in between Jiuquan and the Qaidam Basin, up to 300 km.
最宽处在酒泉市与柴达木盆地之间，达300千米。
Widest point in Jiuquan City and between the Qaidam Basin, 300 km.
柴达木盆地的察尔汗盐湖是典型的干旱地区封闭湖泊。
Qarhan Salt lake is a typical closed lake in the dry Qaidam basin.
用航磁资料研究了青海柴达木盆地中部的深部构造环境。
The deep tectonics in central Tsaidam Basin has been studied with aeromagnetic date.
柴达木盆地阿尔金斜坡中段，是寻找隐蔽油气藏的有利地区之一。
The medium section of Altun slope in Qaidam basin is one of the favourable areas in the exploration of subtle petroleum reservoirs.
通过对柴达木盆地锶资源的综合评价，提出了锶资源的开发方向。
Through the comprehensive evaluation of strontium resources in Chaidamu basin, the development direction of strontium resources is stated.
分析柴达木盆地绿洲形成条件，首次进行柴达木盆地的绿洲区划。
This paper analyses the formative condition for oasis in the Qaidam Basin and carries out the oasis regionalization at first time in the Qaidam Basin.
其中，柴达木盆地的矿产资源最为丰富，建有一批新兴的工业企业。
Meanwhile, there are many new industries in Qaidam Basin because of its rich mineral resources.
柴达木盆地中草药资源比较丰富，具有很高的开发利用价值和潜力。
Chinese medicine resource is abundance and high value of developing utilization in Chaidamu basin.
探讨了适于柴达木盆地难采储量开发的技术措施与针对性、适应性。
The authors explore the measurements, strategies and suitability for the reserve in the basin.
这一发现对于柴达木盆地第三系油气的勘探开发具有重要的实践意义。
This discovery is of important and practical significance for the oil exploration and development in the Qaidam basin.
柴达木盆地和酒泉、肃北旋转方向的差异预示了两地区间存在左旋错动。
The opposite rotation direction implies the existence of left lateral dislocation between Qaidam basin and Jiuquan and Subei areas.
柴达木盆地阿尔金山东南缘地质历史上经历了多期构造运动，构造复杂。
The southeast margin of Aljin mountains in Chaidam basin experienced multi-period structural movement in geologic history, resulted in complex structures.
文章介绍了青海省柴达木盆地盐湖矿产资源的概况、特点以及开发利用现状。
The paper introduces the general situation of exploitation and utilization of salt lake mineral resources in the Chaidamu basin of Qinghai province.
高分辨率地震资料表明，柴达木盆地三湖地区第四系气藏周围发育有气烟囱。
The high resolution seismic data show that gas chimneys exist around Quaternary gas reservoirs in Sanhu area of Qaidam basin.
柴达木盆地东部第四系生物气源岩有机质丰度是控制该区生物气资源的关键因素。
Organic matter abundance of quaternary source rock of biogenic gas in eastern Qaidam basin is the key factor controlling biogenic gas resource in the area.
我国盆地很多，其中大盆地有四川盆地、塔里木盆地、准噶尔盆地和柴达木盆地。
Many of our basin, a large basin with Sichuan basin, Tarim and Junggar basin and Qaidam basin.
柴达木盆地北缘是柴达木盆地三大油气区之一，其源岩为早、中侏罗世煤系地层。
The northern edge in Qaidam Basin is one of the three hydrocarbon bearing areas in the basin. Its source rock is the early and middle Jurassic coal measures.
柴达木盆地石炭系主要分布在柴东地区，是该盆地勘探和研究程度较低的层系之一。
It is one of the stratums which are lower degree of exploration and research in the Qaidam basin.
本文采用频谱分析对柴达木盆地三湖地区第四系自然伽马测井曲线进行了系统分析。
In this paper, the gamma-ray curves of the Quaternary of Sanhu area in eastern Qaidam Basin are analyzed using frequency spectrum analysis method.
柴达木盆地柴西南第三系为一套拗陷湖盆沉积地层，具备形成岩性圈闭的地质条件。
The Tertiary in Qaixinan of Qaidam basin is a set of depressed lake basin sedimentary strata that have geologic condition forming lithologic traps.
柴达木盆地东部地区是第四纪的沉积与沉降中心，内陆湖泊相的沉积厚度大、分布广泛。
The eastern part region of Qidam basin is a Quaternary depositional and subsidence center being large and extensively distributed.
与现代叠层石的对比进一步明确了新生代柴达木盆地湖相叠层石的沉积特点和属性特征。
Compared with the modern stromatolites, the Neogene stromatolites in the Qaidam Basin was further elucidated in sedimentation and features.
柴达木盆地在中国大地构造格局中，处于阿尔金山、祁连山与昆仑山断褶带组成的三角区域。
Chaidam Basin locates in the triangle region that consists of Aerjin mountain, Qilian mountain and Kunlun mountain fault fold belt in the earth structure of China.
柴达木盆地在中国大地构造格局中，处于阿尔金山、祁连山与昆仑山断褶带组成的三角区域。
Chaidam Basin locates in the triangle region that consists of Aerjin mountain, Qilian mountain and Kunlun mountain fault fold belt in the earth structure of China.
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