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Trace Element Geochemistry of Magnetite from the Fe(-Cu) Deposits in the Hami Region, Eastern Tianshan Orogenic Belt, NW China
HUANG Xiaowen; QI Liang; MENG Yumiao
2014
发表期刊Acta Geologica Sinica
卷号88期号:1页码:176-195
摘要

Laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) was used to determine the trace element concentrations of magnetite from the Heifengshan, Shuangfengshan, and Shaquanzi Fe(-Cu) deposits in the Eastern Tianshan Orogenic Belt. The magnetite from these deposits typically contains detectable Mg, Al, Ti, V, Cr, Mn, Co, Ni, Zn and Ga. The trace element contents in magnetite generally vary less than one order of magnitude. The subtle variations of trace element concentrations within a magnetite grain and between the magnetite grains in the same sample probably indicate local inhomogeneity of ore-forming fluids. The variations of Co in magnetite between samples are probably due to the mineral proportion of magnetite and pyrite. Factor analysis has discriminated three types of magnetite: Ni-Mn-V-Ti (Factor 1), Mg-Ai-Zn (Factor 2), and Ga-Co (Factor 3) magnetite. Magnetite from the Heifengshan and Shuangfengshan Fe deposits has similar normalized trace element spider patterns and cannot be discriminated according to these factors. However, magnetite from the Shaquanzi Fe-Cu deposit has affinity to Factor 2 with lower Mg and Al but higher Zn concentrations, indicating that the ore-forming fluids responsible for the Fe-Cu deposit are different from those for Fe deposits. Chemical composition of magnetite indicates that magnetite from these Fe(-Cu) deposits was formed by hydrothermal processes rather than magmatic differentiation. The formation of these Fe(-Cu) deposits may be related to felsic magmatism.

关键词Trace Elements Magnetite La–icp–ms Fe(–cu) Deposits Eastern Tianshan Orogenic Belt Xinjiang
学科领域矿床地球化学
语种英语
文献类型期刊论文
条目标识符http://ir.gyig.ac.cn/handle/352002/5217
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
推荐引用方式
GB/T 7714
HUANG Xiaowen,QI Liang,MENG Yumiao. Trace Element Geochemistry of Magnetite from the Fe(-Cu) Deposits in the Hami Region, Eastern Tianshan Orogenic Belt, NW China[J]. Acta Geologica Sinica,2014,88(1):176-195.
APA HUANG Xiaowen,QI Liang,&MENG Yumiao.(2014).Trace Element Geochemistry of Magnetite from the Fe(-Cu) Deposits in the Hami Region, Eastern Tianshan Orogenic Belt, NW China.Acta Geologica Sinica,88(1),176-195.
MLA HUANG Xiaowen,et al."Trace Element Geochemistry of Magnetite from the Fe(-Cu) Deposits in the Hami Region, Eastern Tianshan Orogenic Belt, NW China".Acta Geologica Sinica 88.1(2014):176-195.
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