%0 Journal Article
%T Sulfides in mantle xenoliths of Cenozoic basalts from Liuhe, Jiangsu province, China.<br>江苏六合新生代玄武岩中地幔捕虏体的硫化物相研究
%A Xu Jiuhu
%A Chu Xuelei
%A Xie Yuling
%A Liu Yan Resource Engineering School
%A University of Science
%A Technology Beijing
%A Beijing
%A Chin
%A Research Center of Mineral Resources Exploration
%A <br>徐九华
%A 储雪蕾
%J 岩石学报
%D 2000
%I 
%X Mantle xenoliths captured in alkali basalt occurs widely in the Liuhe district, Jiangsu province, China, dominantly by spinel lherzolite. Sulfides are commonly found in minerals of the mantle xenoliths. They occur as: (1) early sulfide grains captured by host minerals; (2) intergranular or filling in the fissures; and (3) sulfide melt inclusions, including one phase sulfide inclusions, sulfide glass two phase melt inclusions, and CO 2 sulfide glass (sometimes containing silicate daughter minerals) poly phase melt inclusions. Electron microprobe analysis shows that sulfide melt inclusions have higher Fe and S contents and lower Ni content than sulfides in fissures do. The molar ratios of Ni to Fe, r Ni / r Fe , of sulfide melt inclusions range from 0.14 to 1.73, generally from 0.70 to 1.55, while those of intergranular sulfides range from 1.76 to 7.03 . Like that of Liuhe, sulfide melt inclusions in Hannuoba (Hebei province), Xinchang (Zhejiang province) and Qilin (Guangdong province) have higher Fe and S contents and lower Ni content when compared to intergranular sulfides. For both sulfide melt inclusions and intergranular sulfides, S contents increase from Liuhe, Xinchang, and Hannuoba to Qilin, Fe contents increase from Liuhe, Xinchang, Qilin, to Hannuoba; while Ni( Co) contents decrease from Liuhe, Xinchang, Qilin, to Hannuoba. It is indicated that there is a close relationship between intergranular sulfides and sulfide melt inclusions.
%K Mantle xenolith
%K Sulfides
%K Electron microprobe
%K Liuhe<br>地幔岩
%K 硫化物相
%K 新生物
%K 玄武岩
%K 地幔捕虏体
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=2013B5467E3054B1614CEC199353FCED&aid=09E362ADEBB0564A&yid=9806D0D4EAA9BED3&vid=7801E6FC5AE9020C&iid=E158A972A605785F&sid=4A2356A1257A12EB&eid=E3C3E274D87A8C16&journal_id=1000-0569&journal_name=岩石学报&referenced_num=13&reference_num=8