1) Chaidamu Experiment Area
柴达木试验区
1.
Researches on Circular Economy Developing in Qinghai Chaidamu Experiment Area;
青海柴达木试验区循环经济发展研究
2) Area of Chaidamu
柴达木地区
1.
Culture Technique on Lycium barbarum in Area of Chaidamu;
柴达木地区宁夏枸杞栽培技术
3) Chaidamu
柴达木
1.
Research into the Taijinaier Surname of the Mongolians in the Chaidamu Areas of Qinghai Province;
柴达木台吉乃尔蒙古族姓氏研究
2.
Study on Integrated Propagation and Afforestation Techniques of Drought-Tolerant Species and Afforestation in Chaidamu Area;
柴达木地区抗旱树种繁育及造林综合技术研究
3.
Chinese medicine resource is abundance and high value of developing utilization in Chaidamu basin.
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。
4) Qaidam
柴达木
1.
Consideration on the Sustainable Development of Qaidam's Salt Lake Industry;
对柴达木盐湖产业可持续发展的思考
2.
Depositional systems and filling patterns of the Tertiary Qaidam lake basin in the Ganchaigou region, Qinghai;
柴达木盆地干柴沟地区第三系湖盆边缘斜坡带沉积体系及湖盆充填模式分析
3.
Evolution and dynamics of the Qaidam Tertiary transform rift basin in Qinghai;
柴达木第三纪转换裂陷盆地形成演化及动力学
5) Chai damu
柴达木
1.
The mineral resources of Chai damu basin is quite abundant, but due to that it has been in vulgar management, the efficiency of exploiting and comprehensive reciprocation from resources are low.
柴达木盆地矿产资源丰富,但开发利用效率低,基本上是粗放式经营,资源综合回收率低。
2.
Chai damu basin s minerals resource affluent,in a long period of time,it has basically been run with vulgar way、 exploited with wasting way,and the resource has not been able to be exploited comprehensively.
柴达木盆地矿产资源丰富,长期以来基本上是粗放式经营、浪费式开采,资源没有很好地综合开发利用。
6) Qaidam basin
柴达木
1.
The research of hydrocarbon indication on gas reservior of Qaidam basin;
柴达木盆地第四系气藏烃类检测研究
2.
Narengele drainage system,originated from Kunlun mountains in eastern Qaidam basin,has formed Na-Tuo groundwater circulation system in Pliocene and Pleistocene periods in Wutumeiren,east to Tainan,Sebei and Tuofengshan areas;and on its both sides,Dabuxun Lake subsag and Yiliping subsag are catchment basins characterized by stagnant hydrogeology.
柴达木盆地东部昆仑山脉的那仁格勒河水系在乌图美仁 -台南东 -涩北 -驼峰山地区上新统 -更新统形成了那 -驼地下水循环系统 ,其两侧的达布逊湖洼陷和一里坪洼陷区属汇水盆地性质的停滞水文地质特征。
3.
According to the analysis of multi parameter hydrocarbon geochemical indicators,Hulushan structure in Qaidam Basin could be divided into 3 geochemical abnormal zones:the first abnormal zone is around Husheng 1 Well with an area of 45 km\+2.
采用多参数油气地化指标综合分析 ,柴达木盆地葫芦山构造可划分出 3个化探异常区 :Ⅰ号异常区位于葫深 1井周围 ,面积约 45km2 ,游离烃、酸解烃及ΔC均有异常 ,且叠置吻合性好 ;Ⅱ号异常区位于构造北部 ,主要为游离烃异常 ;Ⅲ号异常区位于测区的东南角 ,规模较小 ,除游离烃甲烷外 ,其他异常均较弱。
补充资料:柴达木游览区
柴达木盆地是青藏高原上地势最低的断线盆地,地理环境以干旱为特征,地貌由周边向中心依次呈现高山,风蚀丘陵,戈壁、沙漠和湖沼五个环带状结构,境内主要旅游景区(点)有察尔汗盐湖及“万丈盐湖”、南八仙、大风山一带的雅丹地区,德合哈柏瀑布,达布旦温泉、达布逊湖“湖中湖”、茶卡柯柯盐湖、巴隆国际狩猎场等,还有新兴的城镇和绿洲是开展“万丈盐桥”、“戈壁沙漠”、“雅丹在貌”、“绿洲农业”观光、狩猎和民俗考察等旅游活动的好地方。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。