2) North Qinling area
北秦岭地区
3) north and south sides of the Qinling Mountain
秦岭南北
1.
Influences of different disaster inducing factors on droughts and floods on the north and south sides of the Qinling Mountain are calculated and analyzed by using the model of drought and flood indexes.
运用旱涝指数模型,计算、分析了不同诱灾因子对秦岭南北旱涝灾害影响。
4) the North Qinling region of Henan
河南北秦岭
5) Qinling region
秦岭地区
1.
Au deposits occur in the low-grade metamorphic areas in Qinling region.
秦岭地区金矿分为南带和北带,在阐述各带大中型矿床成矿特点的基础上,提出了进一步的找矿方向和找矿标志。
2.
There have been some new views about the metallogenic geological conditions of three important types of gold deposits Baguamiao,Maanqiao and Jianchaling in Qinling region.
以上研究为秦岭地区金矿找矿指出了新方向和新类
3.
On the basis of the metallogenic geological background, new technologies and methods for prognosis of the three important types of gold depositsBaguamiao, Shuangwang and Jianchaling, in the Qinling region, western China are presented in this study.
本文以西部秦岭地区八卦庙、双王、煎茶岭 3种重要类型金矿床为例 ,在成矿地质背景研究基础上 ,开展若干新方法新技术的找矿试验 ,研究发现 ,八卦庙式金矿岩石的烃含量与其金品位大致成正相关关系 ;而且金矿化强度和规模越大 ,相关系数值也越大 ;据此根据石英脉的烃含量对隐伏金矿床 (体 )和金矿化规模进行预测。
6) Qinling area
秦岭地区
1.
Lamprophyre is widely distributed in the Qinling area.
秦岭地区煌斑岩广泛分布,大部分蚀变煌斑岩型金矿发现于徽成盆地南侧。
2.
Both the Qinling area and Yunnan-Guizhou-Guangxi contiguous area are important areas where micro- and fine-grained disseminated gold deposits are distributed.
秦岭地区和滇黔桂接壤区均是中国微细浸染型金矿最重要的分布区之一,两地金矿的某些特征相似,均属沉积改造型金矿床,但由于所处的大地构造位置和地质构造演化历程不同,在地质地球化学等方面还存在许多差异。
3.
According to the deposit which has Se element enriched of Qinling area, it has concluded the distributing characteristics and application of the rich Se deposit,as well as the forming mechanism with Se element ore-forming model.
根据秦岭地区富硒矿床的发现,总结了富硒矿床分布特征与应用及其形成的机制与硒元素成矿模式,最后提出了找矿方向。
补充资料：太平洋地区标准会议标准(见太平洋地区标准会议)
太平洋地区标准会议标准(见太平洋地区标准会议)
standards of PASC: see Pacific Area Standards Congress; PASC
Ta iPingyang Diqu Bioozhun Hu呼ib沁幻Zhun太平洋地区标准会议标准(s切md田心sofR巧C)见太平洋地区标准会议。
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