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Resource evaluation of indium in the Dajing tin-polymetallic deposits, Inner Mongolia, China

文献类型：期刊论文

作者Ishihara, Shunso1; Qin, Kezhang2; Wang, Yuwang3
刊名RESOURCE GEOLOGY
出版日期2008
卷号58期号:1页码:72-79
关键词China Dajing indium Inner Mongolia polymetallic tin
ISSN号1344-1698
DOI10.1111/j.1751-3928.2007.00044.x
文献子类Article
英文摘要Individual ores of 37 specimens and five mill concentrates were analyzed chemically, and anomalous indium contents were detected in the tin-polymetallic veins of the Dajing mine. The indium contents are heterogenously distributed (0.5-296 ppm In), and are low generally in the ores of the East Block. Indium is mainly correlated with copper, partly with zinc in the Dajing deposits, implying that the element is substituted in copper and zinc sulfides and sulfosalts. The total indium content is expected as > 768 tons, which is lower than a previous estimation of this mine. The whole tonnage of the southern part of the Da Hinggang Mountains is > 1200 tons In, which is the second largest in China after the tin-polymetallic deposits in the southern China.
WOS关键词DA HINGGAN MOUNTAINS ; MINERALIZATION ; AREA ; ZONE
WOS研究方向Geology ; Mineralogy
语种英语
WOS记录号WOS:000252814300005
出版者BLACKWELL PUBLISHING
源URL[http://ir.iggcas.ac.cn/handle/132A11/68736]  
专题中国科学院地质与地球物理研究所
通讯作者Ishihara, Shunso
作者单位1.AIST, Geol Survey Japan, Tsukuba, Ibaraki 3058567, Japan
2.Chinese Acad Sci, Inst Geol & Geophys, Beijing, Peoples R China
3.Beijing Inst Geol Mineral Resources, Beijing, Peoples R China
推荐引用方式
GB/T 7714		 Ishihara, Shunso,Qin, Kezhang,Wang, Yuwang. Resource evaluation of indium in the Dajing tin-polymetallic deposits, Inner Mongolia, China[J]. RESOURCE GEOLOGY,2008,58(1):72-79.
APA Ishihara, Shunso,Qin, Kezhang,&Wang, Yuwang.(2008).Resource evaluation of indium in the Dajing tin-polymetallic deposits, Inner Mongolia, China.RESOURCE GEOLOGY,58(1),72-79.
MLA Ishihara, Shunso,et al."Resource evaluation of indium in the Dajing tin-polymetallic deposits, Inner Mongolia, China".RESOURCE GEOLOGY 58.1(2008):72-79.

入库方式： OAI收割

来源：地质与地球物理研究所

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