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1)  Aershan City
阿尔山市
1.
Using mathematical statistics method,this paper analyse and forecast the water carrying capacity in Aershan City.
应用数理统计的方法,对阿尔山市水资源承载能力进行分析和预测,表明该市水资源总量较丰富,能够满足近50年经济和城市发展的需求。
2)  Altyn Mountain
阿尔金山
1.
Mesozoic paleocurrent properties in the southern edge of Altyn Mountain in the western Qaidam Basin;
柴西阿尔金山南缘中生界古流特征
2.
Tectonic Attribution and Movement Characteristic of Altyn Mountain;
阿尔金山的构造归属及其构造运动特征
3.
Advance in study of Mesozoic-Cenozoic uplift history of the Altyn Mountains;
阿尔金山中-新生代隆升历史研究进展
3)  Altay Mountains
阿尔泰山
1.
Discovery of the Kumasu gold polymetallic deposit in the Nurt area, Altay Mountains, and ore prospect evaluation;
阿尔泰山诺尔特地区库马苏金多金属矿的发现及找矿前景
2.
REE geochemistry of Qiaoxiahala type Fe-Cu deposits in southern margin of Altay Mountains, Xinjiang, and its geological implications;
新疆阿尔泰山南缘乔夏哈拉式铁铜矿床稀土元素地球化学特征及其地质意义
3.
Metal logeny of Polymetallic Metal logenic Belts on the Southern Margin of the Altay Mountains, Xinjiang,China;
新疆阿尔泰山南缘多金属成矿带的成矿规律
4)  Altun mountains
阿尔金山
1.
Early Paleozoic Magmatism and Gold Metallogenesis in Altun Mountains, Northwest China;
阿尔金山早古生代岩浆活动与金成矿作用
2.
Sedimentary geochemistry and significance of the Middle and Lower Jurassic strata in the frontal areas of the Altun Mountains,Qinghai;
柴西阿尔金山前下中侏罗统沉积地球化学特征及意义
5)  Altyn tagh
阿尔金山
1.
Lower-middle Jurassic distribution and oil-gas exploration direction on the southern Altyn tagh in the western Qaidam Basin;
柴西阿尔金山前中、下侏罗统展布及油气勘探方向
2.
Geothermochronology and tectonic evolution of Eastern Altyn Tagh Mountains,Northwestern China
阿尔金山东段地质热年代学与构造演化
3.
It is concluded that the different order structures in Altyn Tagh fault system controlled the spatial distribution of metallogenic belts,ore fields and ore deposits.
阿尔金走滑断裂系不同级次构造控制阿尔金山地区铜、金成矿带、矿田及矿床的分布 ,区域上可以划分为阿尔金北缘金—铜—铁多金属成矿带和阿尔金铁—铜—金多金属成矿带。
6)  Altun mountain
阿尔金山
1.
Available surface water resources and potential of water development in the Altun mountains and the Qiangtang Plateau;
阿尔金山羌塘高原区域地表水可利用量及开发潜力分析
2.
Three alkali-rich intrusive rock belts in Kunlun Mountain and Altun Mountain area;
昆仑山-阿尔金山地区的三条富碱侵入岩带
3.
Structural Features of the Altun Mountain and Its Fault Systems During Mesozoic and Cenozoic;
中、新生代阿尔金山及其断裂系统的构造性质
补充资料:阿尔山无底洞

无底洞位于阿尔山温泉街东南28公里处的白狼镇境内,为天然山洞,洞口直径3米左右,呈45度角斜入,洞口每到冬季喷云吐雾,恍若仙境。洞深30余米处,山洞陡然直下,深不可测,至今洞深无人知晓,人们称之为无底洞。

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