CORRELATION BETWEEN δD AND H_2O IN SOME GRANITOID OF CHINA

作     者：于津生 虞福基 覃振蔚 YU JIN-SHENG;YU FU-Jl;QIN ZHEN-WEI Guiyang Institute of Geochemistry. Academia Sinica. Guiyang 550002. PRC

作者机构：Guiyang Institute of Geochemistry. Academia Sinica. Guiyang 550002. PRC 

出 版 物：《Science China Chemistry》 (中国科学（化学英文版）)

年 卷 期：1989年第32卷第11期

页      面：1383-1392页

核心收录：

学科分类：07[理学] 0703[理学-化学] 

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

主　　题：granitoid 

摘      要：The correlation between δD and H_2O content in granitoid can be divided into threetypes: closed-system crystallization type (Darongshan type): a flat positive linear corre-lation; open-system degassing type (Laoshan type): a nearly vertical linear positive cor-relation; meteoric hydrothermal exchange type (Gabug type): an irregular negative trendcorrelation.