片理
一些矿物在变质岩中成层状相互平行和近于平行的定向排列所显示的特点。此层状面称为片理面，可以是平直的面，也可以是波状的曲面，岩石极易沿着片理面劈开，片理构造是变质岩中最常见，最具有特征性的构造，通常又可分为片麻构造、片状构造、千枚构造、板状构造和条带状构造。
73
Alias
Contributor
contributed at 2011-12-23
Classification(s)
●
Earth System(in Chinese) Geology
Detailed Description
| English |
|---|
| Name | schistosity |
| Chinese |
|---|
| Name | 片理 |
| Description | 一些矿物在变质岩中成层状相互平行和近于平行的定向排列所显示的特点。此层状面称为片理面，可以是平直的面，也可以是波状的曲面，岩石极易沿着片理面劈开，片理构造是变质岩中最常见，最具有特征性的构造，通常又可分为片麻构造、片状构造、千枚构造、板状构造和条带状构造。 |
How to Cite
NNU_Group (2011). 片理, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/81611889-5b4c-4fb9-a88f-614daa58b720
Copy
Copyright and Disclaimer
All copyrights of a material (model, data, article, etc.) in the OpenGMS fully belong to its author/developer/designer (or any other wording about the owner). The OpenGMS takes every care to avoid copyright infringement, contributor(s) should carefully employ materials from other sources and give proper citations.
