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《GEOCHIMICA》 1996-04
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CARBON ISOTOPIC EVIDENCE FOR THE ORIGIN OF THE SPHERICAL GRAPHITE IN A GRANITE-HOSTED GRAPHITE DEPOSIT, SUJIQUAN, XINJIANG,CHINA

ZhangGuoxin;HuAiqin;ZhangHongbin;ZhangQianfeng ShenYoulin (Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640)  
The graphite deposit in Sujiquan, Xinjiang occurred in Hercynian granite is characterized by the unique spherical structrue of the graphite.The deposit has the δ13C values ranging from -20.5‰ to -23.9‰ with an average of -22.0‰.The carbon isotopic data indicate an organic origin of carbon in the graphite deposit. The deposit is thought to be resulted from the assimilation of the Middle Carboniferous carbonaceous sediments by the Middle Hercynian granite. Boiling and rolling of the assimilated carbon in the intruding granitic magma may account for the spherical structure of the graphite.
【Fund】: 国家自然科学基金 中国科学院地球化学研究所矿床地球化学开放实验室资助
【CateGory Index】: P619.252
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