| CORRELATION BETWEEN δD AND H_2O IN SOME GRANITOID OF CHINA |
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| 作者姓名： | 于津生 虞福基 覃振蔚 |
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| 作者单位： | Guiyang Institute of Geochemistry. Academia Sinica. Guiyang 550002. PRC，Guiyang Institute of Geochemistry. Academia Sinica. Guiyang 550002. PRC，Guiyang Institute of Geochemistry. Academia Sinica. Guiyang 550002. PRC |
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| 基金项目： | Project supported by National Natural Science Foundation of China. |
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| 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.
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