How High Are the P-T Conditions for Paleoproterozoic Metamorphism of the Huangtuling Felsic Granulite, North Dabieshan, Central China?  

作　　者：陈能松 龚松林 孙敏 杨勇 刘嵘 

机构地区：[1]Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China [2]Department of Earth Sciences, The University of Hong Kong, Pokfulam Road, Hong Kong [3]School of Foreign Language, China University of Geosciences, Wuhan 430074, China

出　　处：《Journal of China University of Geosciences》2006年第4期291-301,共11页中国地质大学学报（英文版）

基　　金：This paper is supported by the Special Doctoral Grant of the Ministry ofEducation of China(No.98049114)and the National Natural Science Foundation of China(No.49972023).

摘　　要：This paper is supported by the Special Doctoral Grant of the Ministry of Education of China （No. 98049114） and the National Natural Science Foundation of China （No. 49972023）.This paper is supported by the Special Doctoral Grant of the Ministry of Education of China （No. 98049114） and the National Natural Science Foundation of China （No. 49972023）.

关 键 词：close-to peak garnet growth zoning garnet-Opx thermobarometry peak P-T conditions Palcoproterozoic HP-UHT granulite DABIESHAN assembly event of supercontinent 

分 类 号：P578[天文地球—矿物学]