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1)  Liupanshan Basin
六盘山盆地
1.
Mesozoic Geological Characteristics and Hydrocarbon Exploration Direction in Liupanshan Basin;
六盘山盆地中生界地质特征与油气勘探方向
2.
Geochemistry of hydrocarbon source rocks in the Liupanshan basin at the northeastern margin of the Qinghai-Tibet Plateau;
青藏高原东北缘六盘山盆地烃源岩的地球化学特征
3.
Formation and modification history of the Liupanshan basin on the southwestern margin of the Ordos block and tectonic stress field evolution;
六盘山盆地形成和改造历史及构造应力场演化
2)  the northern part of Liupanshan Basin
六盘山盆地北部
1.
Based on the theory of petrolrum system, this article makes an analysis on the formation and evolution process of the Mz petroleum system in the northern part of Liupanshan Basin, as well as the pre-sent characteristics of Mz petroleum system, which guides the petroleum exploration in this area.
该文运用含油气系统理论,分析六盘山盆地北部中生界油气系统形成演化过程,以及现今盆地北部中生界油气系统特征,并以此指导该地区的中(新)生界油气勘探。
3)  Minhe-Liupanshan basins
民和-六盘山盆地
1.
Minhe-Liupanshan basins are located in the same structural belt of Hexi aisle and belong to the same south edge of ancient continent in north of China,among them Liupanshan basin is the eastward-extending part of the basins in Hexi aisle,both of them have very good geological conditions of petroleum.
民和-六盘山盆地同处河西走廊构造带,同属华北古大陆的南缘,六盘山盆地是河西走廊诸盆地的东延部分,二者地处我国东部构造域和西部构造域的过渡带,都有着很好的石油地质条件,喜山期的旋卷构造,不仅产生了盆地群内盆地的轴向自北西向近南北向的偏转,在盆地内也产生了相应的旋卷构造变形,早期的钻探都集中在靠近旋扭核部,都产生了"口口见显示,口口不流油"的现象。
4)  the Liupanshan region
六盘山地区
1.
In this paper the formation conditions of interlayer oxidation zone sandstone type copper(uranium) deposits in the Liupanshan region are analyzed from the stratigraphic basin,geochronologic and geochemical environment,the target horizon,epigenetic aiteration,as well as hydrogeological conditions.
从盆地结构、岩相古地理环境,找矿目的层、后生蚀变及水文地质等方面,分析了六盘山地区层间氧化带砂岩型铜(铀)矿的形成条件,认为该地区有利于形成层间氧化带砂岩型铜(铀)矿化,是一个值得进一步探索的地区。
5)  Liupanshan area
六盘山地区
1.
The hard soil and soft rock is one kind of special weak rocky soil which in the Ningxia Liupanshan area highway construction often meets, it has the adverse effect to the road side slope stability.
硬土软岩是宁夏六盘山地区公路建设中常遇到的一种特殊软弱岩土,它对公路边坡的稳定性有不利影响。
6)  Qilian Mt.-Liupan Mt. earthquake belt
祁连山-六盘山地震带
补充资料:六盘山
六盘山

    跨中国宁夏、甘肃、陕西3省区,为近南北走向的狭长山地。南段又称陇山。六盘山海拔2000~2500米,主峰六盘山2928米,在宁夏固原县、隆德县境。由平凉至宁静的公路经此,山路曲折险狭,古代盘道须经六重盘道始达山顶,故名。最高峰米缸山海拔2942米。六盘山为陕北黄土高原与陇中黄土高原界山,亦为泾河与渭河水系的分水岭。山地为强烈地震带,1920年海原县曾发生8.5级地震。
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