1) ductile shear deformation
韧性剪切变形
1.
Constraints of ductile shear deformation on rock geochemical behavior-an example from the Bashikaogong ductile shear zone in the northern Altyn Tagh;
韧性剪切变形对岩石地球化学行为的制约——以北阿尔金巴什考供韧性剪切带为例
2.
The characteristics of the ductile shear deformation developed between the Neoarchaeozoic Se erdengshan Group,and Neoarchaeozoic to Paleoprozoic gneissic tonalite (the basement),and the Dulahala and Jianshan formations of the Baiyun ebo Group ,and the Shujigou and Zenglongchang formations of the Zha ertaishan Group, Changcheng System (the cover)are identical.
内蒙古中部新太古界色尔腾山岩群、新太古代和古元古代片麻状英云闪长岩(基底岩系)与白云鄂博群长城系都拉哈拉组、尖山组和渣尔泰山群长城系书记沟组、增隆昌组(盖层)之间的韧性剪切变形特征相同。
2) brittle-ductile shearing deformation
脆韧性剪切变形
3) malleable shear deformable body
韧性剪切变形带
1.
The long large malleable shear deformable body in Gaowu area has different types and the geologic characters are distinctive.
从江高武地区长冲大型韧性剪切变形带变形样式多样,地质特征独具特色,反应了该区剪切变形带经历塑性变形-脆性变形过程。
4) ductile shear zone with deformation and metamorphism
韧性剪切变形变质带
5) Ductile rheologic shear
韧性-流变剪切
6) ductile shearing
韧性剪切
1.
Simulating experiments were done on foe migration process- "releasing local migration" of SiO2 in phyllite in the process of ductile shearing.
实验较好地模拟了韧性剪切作用过程中SiO2“释放-局部迁移”的迁移过程。
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。 |
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参考词条