Determination of serpentine dehydration temperature at 1- 5 GPa by the method of electrical conductivity  

作　　者：宋茂双 谢鸿森 郑海飞 郭捷 徐有生 许祖鸣 

机构地区：[1]Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China [2]Department of Geology,Peking University Beijing 100871,China

出　　处：《Chinese Science Bulletin》1996年第21期1815-1819,共5页

基　　金：Project supported by the National Natural Science Foundation of China.

摘　　要：The stable fields of hydrous minerals are very important for us to inquire into dia-genesis,magmatism,metamorphic evolution and geochemical process of subduction zone.Until now,the dehydration temperatures of hydrous minerals at high pressure are mainlydetermined by phase equilibrium experiment,HP-DTA analysis,MD calculation as well

关 键 词：HIGH TEMPERATURE and HIGH pressure SERPENTINE electrical CONDUCTIVITY DEHYDRATION temperature. 

分 类 号：P584[天文地球—岩石学]