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Characteristics and trace element geochemistry of pyrite from the songhu iron deposit, nilek county, xinjiang, china

文献类型:期刊论文

作者Shan Qiang1; Zhang Bing3; Luo Yong1,2; Zhou ChangPing3; Yu XueYuan1; Zeng Qiao Song; Yang WuBin1,2; Niu HeCai1
刊名Acta petrologica sinica
出版日期2009-06-01
卷号25期号:6页码:1456-1464
关键词Songhu iron deposit Pyrite Co content Co/ni ratio Volcanic activity
ISSN号1000-0569
通讯作者Shan qiang(qshan@gig.ac.cn)
英文摘要The songhu iron deposit is located in the eastern part of awurale region, and its bed-like orebodies occurred in the voleanic-pyroclastic rocks of the lower carboniferous awurale formation. the volcanic rocks, as the wall/host rocks of the deposit, were formed in an island arc tectonic setting according to their trace element geochemistry. three genetic types of pyrite have been distinguished in the deposit: the framboidal, the anhedral-subhedral ( with a large amount of pyritized bio-remains), and the cobalt pyrite. the pre-iron ore framboidal pyrite of sedimentary origin recrystallized due to the reworking of ore-forming hydrothermal solution, accompanied by the apparent increasing of its co content and co/ni ratio. the iron ore-stage anhedral-subhedral pyrite and associated pyritized bio-remains possess relatively higher co contents and co/ni ratios, indicating the close relationship between the ore-forming fluid and the magmatic (volcanic) activities. the songhu iron deposit was superimposed by late stage cu-co mineralization, in which a large amount of chalcopyrite and cobalt pyrite were formed. the co content of cobalt pyrite can be over 1% and its co/ni ratio over 26. it is suggested that the process of cu-co enrichment in the deposit is closely related to the latter stage of volcanic activity, this deposit could be recognized as a volcanic exhalative sedimentary iron deposit, and its ore-forming temperature ranges from 270 degrees c to 325 degrees c.
WOS关键词SOLID-SOLUTION MODEL ; SULFIDE MINERALS ; FRAMBOIDAL PYRITE ; GOLD DEPOSITS ; ORE GENESIS ; AUSTRALIA ; CHEMISTRY ; SYSTEMS ; NEVADA ; SULFUR
WOS研究方向Geology
WOS类目Geology
语种英语
WOS记录号WOS:000267571400016
出版者SCIENCE PRESS
URI标识http://www.irgrid.ac.cn/handle/1471x/2394022
专题中国科学院大学
通讯作者Shan Qiang
作者单位1.Chinese Acad Sci, Guangzhou Inst Geochem, Guangzhou 510640, Peoples R China
2.Chinese Acad Sci, Grad Univ, Beijing 100049, Peoples R China
3.Xinjiang Bur Geol & Mineral Resource Explorat, Geol Survey Team 7, Wusu 833000, Peoples R China
推荐引用方式
GB/T 7714
Shan Qiang,Zhang Bing,Luo Yong,et al. Characteristics and trace element geochemistry of pyrite from the songhu iron deposit, nilek county, xinjiang, china[J]. Acta petrologica sinica,2009,25(6):1456-1464.
APA Shan Qiang.,Zhang Bing.,Luo Yong.,Zhou ChangPing.,Yu XueYuan.,...&Niu HeCai.(2009).Characteristics and trace element geochemistry of pyrite from the songhu iron deposit, nilek county, xinjiang, china.Acta petrologica sinica,25(6),1456-1464.
MLA Shan Qiang,et al."Characteristics and trace element geochemistry of pyrite from the songhu iron deposit, nilek county, xinjiang, china".Acta petrologica sinica 25.6(2009):1456-1464.

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来源:中国科学院大学

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