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1)  Mohe ductile shear zone
漠河韧性剪切带
1.
~(40)Ar-~(39)Ar dating of the muscovite in the mylonite of the Mohe ductile shear zone in northern Da Hinggan mountain and its geological significance;
大兴安岭北部漠河韧性剪切带白云母~(40)Ar-~(39)Ar年龄及地质意义
2)  Hetai ductile shear zone
河台韧性剪切带
3)  ductile shear belt
韧性剪切带
1.
Features of ductile shear belt of Xinglong gold mining area and its mineral-bearing potentiality;
兴隆金矿区韧性剪切带特征及其含矿性研究
2.
The formation and distribution of the known gold deposits are both related to ductile shear belts,which are major ore-controlling structure of greenstone type gold deposits.
已知金矿床的形成与分布均与韧性剪切带有关,韧性剪切带是形成绿岩型金矿的主要控矿构造。
3.
The gold deposit of Jinshan is metamorphic hydrothermal solution type which is controlled by the ductile shear belt.
“金山式”金矿床属于受韧性剪切带控制的变质热液型金矿床。
4)  ductile shear zone
韧性剪切带
1.
Ore-controlling characteristics of the ductile shear zone and prospecting perpective in Jiangdongwan gold-antimony orefield, Hunan;
湖南江东湾金锑矿床韧性剪切带控矿特征及找矿前景
2.
Eerguna River ductile shear zone and its relation to gold mineralization in Inner Mongolia;
内蒙古额尔古纳河韧性剪切带与金矿化
3.
Determination of the formation temperature of the earlier ductile shear zone in the Tan-Lu fault zone,eastern Dabie Mountains;
大别山东缘郯庐断裂带早期韧性剪切带的形成温度
5)  ductile shearing zone
韧性剪切带
1.
All the gold is hosted by different parts of the Qiumingtashi-Huashan ductile shearing zone .
通过对新疆红石金矿区韧性剪切变形特征的研究,金矿化带的分布明显受韧性剪切带的控制,所有的金矿体及金矿化体均赋存于秋格明塔什-黄山韧性剪切带的不同部位,其变形期次可划分为3期,即韧性剪切变形、脆-韧性剪切变形和脆性剪切变形,其中脆-韧性剪切变形阶段是最有利的成矿阶段。
6)  ductile shear zones
韧性剪切带
1.
Base on the study about precious metal mineralization and ore-controlling structures, it is realized that ductile shear zones, especially those developed in the Archean granite-greenstone belt, are the most important ore-controlling structures.
国内外贵金属与控矿构造研究表明,韧性剪切带,特别是发育在太古宙古老陆核花岗—绿岩地体中的韧性剪切带是最重要的控矿构造。
2.
Zhilinton gold-siver deposit, surrounded by Proterozoic metamorphic rocks and controlled by the ductile shear zones, is a large one.
治岭头金银矿床是产于浙西南元古界变质地体内的含金韧性剪切带型大型矿床。
3.
Some lower-crust ductile shear zones(DSZ) occurred in Daqingshan area of Inner Mongolia.
内蒙古大青山高级变质杂岩区发育多条近东西向、平行相间排列的深层次韧性剪切带。
补充资料:漠河风光北极村

漠河风光北极村地处北纬53°22′是中国北极边城,江对岸是俄罗斯的依古纳思诺村。

冬季气温达摄氏零下50°,故有“中国北极村”之称。在漫长的冬季里,常可看到绚丽多彩的北极风光。在夏季里,这里几乎没有黑夜,深夜11时,天色尚未全黑,而在凌晨1时又呈现晨光,因此形成有名的“白夜”。

说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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