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1)  the southern slope of the Daxiangling Mountains
大相岭南坡
1.
0 technology support,the study took the southern slope of the Daxiangling Mountains as an example,use the mixed methods of eye-interpretion,supervision and un-supervision to interpret the change of land use and the cover,and then compute the correlation indexes of land use dynamic change and land use conversion matrix.
本文利用大相岭南坡1982年MSS卫片和2006年ASTER卫片,在ArcGIS9。
2)  the southern slope of the Naling Mountains,China
南岭南坡
3)  south slope of Qinling Mountains
秦岭南坡
1.
The authors investigated soil fertility at the Macrocarprim officinalis base of Longcaoping Bureau of Forestry in the main production zone on the south slope of Qinling Mountains,then evaluated soil quality there and classified different categories of growing conditions of macrocarpium officinalis.
对秦岭南坡山茱萸主产区的龙草坪林业局山茱萸基地进行了土壤肥力调查,在此基础上对土地质量进行评价,并划分了立地类型。
4)  the southern slope of Qinling Mountains
秦岭南坡
1.
21 species belonging to 11 genera, 11 families of Lichen from the southern slope of Qinling Mountains were report in this paper.
报道了采自于秦岭南坡的地衣植物21种,隶属于11科、11属。
5)  Nandaling Formation
南大岭组
1.
The Early Jurassic Nandaling Formation in the Vicinity of Shanggu,Chengde of Hebei;
论河北承德上谷早侏罗世南大岭组
2.
species of 12 genera are described here for the first time from the Nandaling Formation near Shanggu, Chengde of Hebei.
描述了河北承德上谷附近门头沟群南大岭组植物化石12属15种,认为其时代为早侏罗世。
3.
The strata in Northwestern Hebei area are divided into Nandaling Formation, Xiahuayuan Formation, Jiulongshan Formation,Tiaojishan Formation and Houcheng Formation while in the western Beijing area the strata that is considered the same layer to the Xiahuayuan Formation are divided into Yaopo Formation and Longmen Formation.
前者划分为南大岭组、下花园组、九龙山组、髫髻山组和后城组,后者与下花园组相当的地层又分为窑坡组和龙门组。
6)  Lingnan University
岭南大学
1.
A tentative study of funds-raising of Lingnan University and its influencing factors;
岭南大学经费筹措及其影响因素分析
2.
Dissertation on Chen Xujing and Lingnan University, Canton (1948-1952);
试论陈序经与岭南大学(1948—1952)
补充资料:大相岭
      大渡河和青衣江的分水岭,四川省南北部重要的自然地理界线。又称相公岭和泥巴山。山体蜿蜒于省境西部雅安、荥经和汉源之间,西靠二郎山,东接峨眉山,走向近北西。南北自然景观迥然不同,历史上即有"清风、雅雨、干富林"之说。山南少雨干燥,植被稀疏,山北多雨湿润,林高草密,是四川突出的多雨区,年降水量可达2400毫米。山体由古生代变质岩、花岗岩和中生代红色砂页组成,富煤、铁、磷、 菱镁矿及铜、铅、 锌、锰、钴。山脊海拔约3000米,最高轿子顶达3552米。川滇西线公路通过的垭口为2552米。大相岭东坡也有大熊猫分布。山南的汉源是四川省花椒主产地,花椒品质历来居全国之冠。
  

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