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Geology and sulfur isotope geochemistry of Dafulou tin-polymetallic deposit in Dachang orefield, Guangxi, China
Yong-sheng Cheng
2013
发表期刊Journal of Central South University
卷号20期号:10页码:2811-2818
摘要No. 22 ore of Dafulou deposit was systematically analyzed for sulfur isotopes. The results show that the δ 34S values of sulfide minerals, ranging from −0.154 to +0.218% and with an average value of +0.114 1%, are mostly positive and characterized by rich sulfur (S) content. This suggests that the sulfur of the Dafulou ore deposit is derived from magma and relates to the Longxianggai concealed granite, which points to the important role of magma during mineralization and implyies the product of the active continental margin. By comparison between the Dafulou and the Kengma tin deposit, significant differences exist in the sulfur isotope composition. In the Kengma deposit, the sulfur isotope composition is characterized by the high negative value, which is different from the Dafulou tin-polymetallic deposit. The difference of the enrichment and fractionation of the sulfur isotope is the synthesized result of the metallogenic conditions. It also has the difference in the metallogenic environment and metallogenic characteristics of the deposit in the same ore belt.
关键词Tin-polymetallic Deposit Sulfur Isotope Ore-forming Material Sources Dafulou Deposit
学科领域矿床地球化学
收录类别SCI
语种英语
文献类型期刊论文
条目标识符http://ir.gyig.ac.cn/handle/352002/4999
专题矿床地球化学国家重点实验室_矿床地球化学国家重点实验室_期刊论文
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Yong-sheng Cheng. Geology and sulfur isotope geochemistry of Dafulou tin-polymetallic deposit in Dachang orefield, Guangxi, China[J]. Journal of Central South University,2013,20(10):2811-2818.
APA Yong-sheng Cheng.(2013).Geology and sulfur isotope geochemistry of Dafulou tin-polymetallic deposit in Dachang orefield, Guangxi, China.Journal of Central South University,20(10),2811-2818.
MLA Yong-sheng Cheng."Geology and sulfur isotope geochemistry of Dafulou tin-polymetallic deposit in Dachang orefield, Guangxi, China".Journal of Central South University 20.10(2013):2811-2818.
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