| 吐哈盆地南缘大草滩韧性剪切带的变形特征及演化 |
| |
| 引用本文： | 白明洲. 吐哈盆地南缘大草滩韧性剪切带的变形特征及演化[J]. 新疆工学院学报, 1997, 18(3): 231-234 |
| |
| 作者姓名： | 白明洲 |
| |
| 作者单位： | 新疆工学院地质系!乌鲁木齐，830008 |
| |
| 摘 要： | 大草滩韧性剪切带岩石变形特征明显，有从强到弱三个程度不同的变形带，它是从晚石炭世初至晚石炭世末期发展起来的，是准噶尔板块和塔里木板块相互作用的结果．
|
| 关 键 词： | 大草滩韧性剪切带 岩石变形 构造演化 |
DEFORMATION CHARACTER AND EVOLUTION OF DACAOTAN DUCTILE SHEAR ZONE ON THE SOUTH MARGIN OF TUHA BASIN |
| |
| Bai Mingzhou. DEFORMATION CHARACTER AND EVOLUTION OF DACAOTAN DUCTILE SHEAR ZONE ON THE SOUTH MARGIN OF TUHA BASIN[J]. , 1997, 18(3): 231-234 |
| |
| Authors: | Bai Mingzhou |
| |
| Affiliation: | Dept. of Geology Urumqi 830008 |
| |
| Abstract: | The character of the rock deformation in Dacaotan ductile shear zone is obvious. Thereare three deformation zones. Dacootan ductile shear zone developed during the late Carbonif-erous period and it's the result of the mutual action between Tarim plate and Junggar plate. |
| |
| Keywords: | Ductile shear zone Rock deformation Structural evolution |
| 本文献已被 CNKI 维普 等数据库收录！ |
