尖灭侧现
扭裂带及压扭性或张扭性断裂带中的低级序破裂面及产于其中的矿脉或岩脉，首尾错开、呈雁行排列的现象。沿走向和倾向都极为普遍，单个脉体延伸方向与整个断裂带有一定交角。据此规律可推知断裂两侧运动方向和预测矿脉分布部位。
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contributed at 2011-10-13
Classification(s)
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Earth System(in Chinese) Geomechanics
Detailed Description
| English |
|---|
| Name | lateral en echelon arrangement(of structures) |
| Chinese |
|---|
| Name | 尖灭侧现 |
| Description | 扭裂带及压扭性或张扭性断裂带中的低级序破裂面及产于其中的矿脉或岩脉，首尾错开、呈雁行排列的现象。沿走向和倾向都极为普遍，单个脉体延伸方向与整个断裂带有一定交角。据此规律可推知断裂两侧运动方向和预测矿脉分布部位。 |
How to Cite
NNU_Group (2011). 尖灭侧现, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/fee3dc93-8272-498e-85b2-44ec4c2e3b3b
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