1) Bairiqili rock body
白日其利岩体
1.
The studies of geological characteristics, melanic inclusion and Nd Sr isotopeshow that the Triassic Bairiqili rock body in the middle sector of East Kunlun was formed bynonhomogeneous and incomplete mixing of crust and mantle magma many times.
通过对岩体地质特征、暗色包体及Nd、Sr同位素资料研究表明:东昆仑中段中三叠世白日其利岩体是由壳幔岩浆不均一或不彻底多次混合作用形成的,岩体内部呈现出酸性、基性岩浆因混合程度和混合比例不同而形成复杂的岩体结构样式,其基性端元为混合不彻底而残留的辉长质岩石,酸性端元是受轻度混染的二长花岗岩,岩浆混合作用方式以就地混合为主,岩体形成于碰撞造山期后的构造环境。
2) Harbaiq Gacha
哈日白其嘎查
1.
The paper has six chapters as introduction,the basic situation of Harbaiq Gacha,the nomadic condition of Harbaiq Gacha,the benefits of nomadism,summary and references.
本文根据政府有关文件以及社会调查材料,细致地阐述了巴林左旗白音乌拉苏木哈日白其嘎查至今还保留三季游牧方式的基本情况,并分析了其原因以及游牧对生态保护和牧民生活的影响。
3) rock mass utilization
岩体利用
4) Dangrous rock-mass
白岩危岩体
1.
Measure and analysis of rock falling scene for Baiyan Dangrous rock-mass over Maoping Landslide,Qinjiang;
清江茅坪滑坡白岩危岩体崩塌现场测量及其分析
5) dolomite mass
白云岩体
1.
The dolomite mass of Tianhuan northern section in Ordos Basin, about 200 km from south to north and 40～80 km from east to west, with 10 000 km~2 area, develop in the middle member 4 of Majiagou formation, mainly distributing in SN along the well Dingtan-1 to well E-6, to western well Bu-1 and well Tian-2, and to eastern well Chengchuan-1.
鄂尔多斯盆地天环北段白云岩体主要发育于马家沟组马四段中,主要沿定探1井~鄂6井呈南北向展布,西部延伸至布1井~天2井一线,东部则到城川1井区,南北长约200km,东西宽约40~80km,总面积约10 000km2,最大厚度达431m。
6) intrusion age
太白岩体
1.
Subdivision of rock series units and determination of intrusion age of Taibai rock mass in North Qinling;
北秦岭太白岩体岩石谱系单位划分及侵位时代确定
补充资料：白日贼
1.指以小商贩为掩护的骗子。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条