The white schist assemblage in the kyanite quartzite from the ultrahigh-pressure metamorphic belt, eastern Dabie Mountains |
| |
Authors: | Laili Jiang Shutong Xu Yican Liu Weiping Wu Wen Su |
| |
Affiliation: | (1) Anhui Institute of Geology, 230001 Hefei, China |
| |
Abstract: | The kyanite quartzite from the ultrahigh-pressure metamorphic belt in the eastern Dabie Mountains is composed mainly of quartz, kyanite, talc and epidote, which contains a typical mineral assemblage of white schist. It suffered an eclogite facies metamorphism ofP = (2.4 ±0.3) GPa andT = 630 ° C together with coexisting eclogite. The protolith may be an aplite replaced by high-pressure fluid of eclogite facies. |
| |
Keywords: | Dabie Mountains ultrahigh pressure white schist assemblage |
本文献已被 SpringerLink 等数据库收录! |
| 点击此处可从《科学通报(英文版)》浏览原始摘要信息 |
|
点击此处可从《科学通报(英文版)》下载全文 |