玻状岩
又称假玄武玻璃。一种由动力变质作用形成的玻璃质岩石。它们是原来岩石在强烈错动产生的高温影响下发生融熔，又经快速冷却所形成。岩石一般为黑色，有时为棕色玻璃或隐晶质，具玻璃结构或部分脱玻化结构，条带状或条纹状构造。常见于扭性或压扭性断裂带，分布范围有限。
31
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contributed at 2011-10-11
Classification(s)
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Earth System(in Chinese) Igneous petrology
Detailed Description
| English |
|---|
| Name | pseudotachylite |
| Chinese |
|---|
| Name | 玻状岩 |
| Description | 又称假玄武玻璃。一种由动力变质作用形成的玻璃质岩石。它们是原来岩石在强烈错动产生的高温影响下发生融熔，又经快速冷却所形成。岩石一般为黑色，有时为棕色玻璃或隐晶质，具玻璃结构或部分脱玻化结构，条带状或条纹状构造。常见于扭性或压扭性断裂带，分布范围有限。 |
How to Cite
NNU_Group (2011). 玻状岩, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/8696e53e-6bc9-4743-a2fc-611ef29f55a6
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