斯图特运动
又称阿得莱德运动(Adelaidean orogeny)。发生于晚元古代末的造山运动，定名于澳大利亚南部阿得莱德地区。那里的阿得莱德系沉积岩受到强烈的逆冲和倒转褶皱。该运动先在南部上升，后来沿岩系的北缘上升。它是根据澳大利亚南部阿得雷德新元古界布拉(Burra)群与其上的翁贝拉塔纳(Umberatana)群之间的角度不整合确定。其发生时限为距今750百万年。
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contributed at 2011-10-12
Classification(s)
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Earth System(in Chinese) Tectonic movement
Detailed Description
| English |
|---|
| Name | Sturian orogeny |
| Chinese |
|---|
| Name | 斯图特运动 |
| Description | 又称阿得莱德运动(Adelaidean orogeny)。发生于晚元古代末的造山运动，定名于澳大利亚南部阿得莱德地区。那里的阿得莱德系沉积岩受到强烈的逆冲和倒转褶皱。该运动先在南部上升，后来沿岩系的北缘上升。它是根据澳大利亚南部阿得雷德新元古界布拉(Burra)群与其上的翁贝拉塔纳(Umberatana)群之间的角度不整合确定。其发生时限为距今750百万年。 |
How to Cite
NNU_Group (2011). 斯图特运动, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/a06546a7-fa59-46b5-b7f6-1b04bb2d5050
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