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《Journal of Changchun University of Science and Technology》 2001-02
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THE CHARACTERISTICS OF FLUID DURING METAMORPHIC PEAK OF THE ARCHEAN KHONDALITE SERIES FROM XINGHE DISTRICT,INNER MONGGOLIA

DONG Yong sheng, ZHOU Xi wen (College of Earth Sciences, Jilin University, Changchun 130026, China)  
For the purpose to demonstrate the nature of fluid during peak metamorphism of the Archean Khondalite series,this paper focus on the carbonic liquid inclusions with negative crystal form within diagnostic mineral-sillimanite of the Archean Kondalite series in the studied regeon.According to the data obtained from micro-thermometer and laser Raman microprobe,the fluid inclusions of this kind are characterized by low x H 2O (0 mol%~17 mol%),very high carbonic materials ( x CO 2+CH 4 =70 mol%~90 mol%), with density 0.94~1.0 g/cm 3 corresponding to pressure about 0.7 GPa. And the fugacity of oxygen (lg f O 2 ) is between -14 and -16. Above evidences show that the abundant carbonic material are not derived from deep source, but probably generated by oxidation of organic material in protolith of the Khondalite series.
【Fund】: 国家自然科学基金!资助项目 (49772 144 )
【CateGory Index】: P588.3
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