1) Xinglongshan Natural Conservation Area
甘肃兴隆山
1.
Eighteen species of powdery mildews ( Erysiphales) from Xinglongshan Natural Conservation Area were collected and identified.
调查了甘肃兴隆山国家级自然保护区白粉菌的资源状况。
2) 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。
3) 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。
4) Guan mountain
甘肃关山
5) Beishan
甘肃北山
1.
A suite of volcanic-sedimentary strata exist in the Herzhadegai area,northern section of Beishan in Gansu Province,which is determined as Saozishan Formation through the study of geological ages and lithostratigraphic and regional correlation,meanwhile,subdivided into 4 lithological members in terms of their lithological differences.
甘肃北山北部霍勒扎德盖地区,分布着一套火山—沉积地层,对其进行岩石地层、区域对比及地层年代等方面的研究,划归扫子山组,并依据组内岩性差异划分为4个岩性段。
6) Beishan area of Gansu
甘肃北山
1.
Age and preliminary revision of the Pochengshan formation in Beishan area of Gansu province;
甘肃北山地区"破城山组"的初步修订和时代
补充资料：兴隆山
原名兴龙山。位于兰州城东南45公里处，属秦祁地轴在陇西高原隆起部分，走向北西，地层属下震旦统兴隆山群。岩性自下至上有安山岩、千枚岩、玄武岩、白云岩、灰岩、板岩等。由龛峪河（大峡河）切割而成的兴隆峡，将山分为东、西两山：东山即兴隆主山，又名争秀山，海拔2816米,山坡有太白泉和玉液泉诸名胜,最高峰九子坪，海拔3130米；西山名栖云山，海拔2524米，上有清代悟元子修道处及仙人洞诸名胜，高峰3021米。两山阴坡均有松、 杉林及青杄、白杨。 植物种类极丰，仅高等植物就达500种以上。半山庙宇多已拆毁,山麓建有休养所等。两山之间由木制拱形握桥──云龙桥相联系。1985年农历6月6日恢复历史传统的游山会。山区建有兴隆山自然保护区，1988年划为国家级自然保护区。
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