2) the Maxian mountain region
甘肃马衔山区
3) Beishan Region
甘肃北山地区
1.
Tectonic Deformation and Evolution Trend of Beishan Region, Gansu Province since Late Quaternary;
甘肃北山地区晚第四纪构造变形特征及演化趋势
4) Beishan of Gansu province
甘肃北山
1.
After that,the authors take Beishan of Gansu province for the HLW disposal area as the example,and measure the joint roughness coefficient(JRC) of surface rock mass and cores of borehole.
文章评述了现有岩体结构面粗糙度系数(JRC)的各种测定方法及存在的问题,分析了在高放废物处置库预选场址甘肃北山花岗岩地区,用"简易纵剖面仪"进行地表岩体及钻孔岩心裂隙结构面JRC的测量结果。
5) Beishan area of Gansu Province
甘肃北山
1.
Using the new achievements of geological survey and the comprehensive materials from previous research and exploration on geology, geophysics, geochemistry and remote sensing, Beishan area of Gansu Province is divided into two gradeⅡ metallogenic zones, three gradeⅢ metallogenic belts and ten gradeⅣ sub-metallogenic belts.
根据成矿地质背景和成矿在时空上的联系性 ,以板块构造单元为基础 ,结合地质、物探、化探、遥感等成矿信息 ,将甘肃北山成矿区带厘定为 2个Ⅱ级成矿区 ,3个Ⅲ级成矿带 ,1 0个Ⅳ级成矿带。
2.
There are some reorganization of sedimentary rock existed in Sinian Xichangjing Group in Beishan area of Gansu Province.
甘肃北山地区震旦纪洗肠井群中留存诸多沉积岩识别标志。
3.
The spatial distribution of Indo-Chinese and Yanshan Epoch granites in Beishan area of Gansu Province are summarized in combination with the features of some typical deposits which metallogenesis are relevant to these granites.
本文讨论了甘肃北山地区印支燕山期花岗岩的空间分布与构造,矿化集中区的耦合关系;与印支燕山期花岗岩活动有成因关系的几个典型矿床;印支燕山期作用强度、构造环境、矿源层和矿化集中区。
6) Guan mountain
甘肃关山
补充资料：鎏金舞马衔杯银壶
鎏金舞马衔杯银壶 盛唐著名银器。1970年陕西西安南郊何家村唐代窑藏出土。通高18.5厘米。这件仿皮囊形银壶，器腹两面均锤出一马衔杯纹，马颈系飘带，昂首扬尾，似作舞状。纹饰鎏金。形制优美，图案别致，制作精工。圈足内有墨书一行：“十三两半”。现藏陕西省博物馆。
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