| 坪上一带深层次构造岩的变形特征及温压条件分析 |
| |
| 引用本文： | 张忠义,丁峰.坪上一带深层次构造岩的变形特征及温压条件分析[J].山东国土资源,2001(Z1). |
| |
| 作者姓名： | 张忠义 丁峰 |
| |
| 作者单位： | 山东省第四地质矿产勘查院 山东潍坊261021
(张忠义)，山东省第四地质矿产勘查院 山东潍坊261021(丁峰) |
| |
| 摘 要： | 山东坪上一带深层次构造岩发育 ,依其塑性变形矿物及其组合、同构造新晶和同构造变形晶所反映的变形特征的不同可分为石英变形相构造岩、钾长石变形相构造岩和斜长石变形相构造岩 ,其变形时的温压条件为中压相系的低绿片岩相—低角闪岩相
|
| 关 键 词： | 深层次构造岩 变形相 温压条件 坪上地区 |
Study on Deep-level Tectonites in Pingshang |
| |
| ZHANG Zhong-yi,DING Feng.Study on Deep-level Tectonites in Pingshang[J].Land and Resources in SHANDONG Province,2001(Z1). |
| |
| Authors: | ZHANG Zhong-yi DING Feng |
| |
| Abstract: | Deep-level tectonites develope well in Pingshang area. According to plastic deformed minerals and their combination, defromed characteristics reflected by synorogenic new crystal and synogenic deformed crystal, they can be divided into quartz deformed tectonites, potash feldspar deformed tectonites and plagioclase deformed tectonites. The deformation temperature and pressure condition are from middle-pressure low greenschist facies to low amphibolite facies. |
| |
| Keywords: | Deep-level tectonites deformed facies temperature and pressure condition Pingshang area |
| 本文献已被 CNKI 等数据库收录！ |
