1) lower crustal ductile shear zone
下地壳韧性剪切带
2) Ductile shearing in deep crust
深地壳韧性剪切作用
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：韧性剪切带
| 韧性剪切带 ductile shear zone 地壳深部(大于10～15千米)具有强烈塑性流变及旋转应变的面状高应变带。又称韧性断层。韧性剪切带中没有明显的不连续面，与两侧岩石之间的应变呈递进演化的关系 ，两侧岩石则显示出明显的剪切位移。规模小者见于显微镜下的薄片中，大者宽数十千米，延展可达上千千米，常见于造山带。韧性剪切带主要地质构造特征有：①面理、线理发育。②应变自中心向两侧递减，由此形成的面理或线理呈连续的S形或反S形排布。③带中岩石具明显的旋转构造特征，如不对称压力影，S型云母鱼。④软性矿物常呈优选方位组构特征。⑤在中心高应变带发育有糜棱岩。⑥在中心高应变带常可见到由于强烈剪切而形成与线理近于平行的A型褶皱或似箭鞘状的鞘褶皱。 |
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