中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
In situ crystallization of Fe-Ti oxides in the Bijigou layered intrusion: Insights from crystal size distributions and compositions of magnetite and ilmenite

文献类型:期刊论文

作者Wang, Mengxi1,3; Zhang, Buqian1; Li, Zhongzhou1; Wang, Jie2,3; Wang, Jiangze2,3
刊名JOURNAL OF ASIAN EARTH SCIENCES
出版日期2023-10-01
卷号255页码:17
关键词In situ crystallization Oxygen fugacity Chromium concentration Fe-Ti oxides Layered intrusions
ISSN号1367-9120
DOI10.1016/j.jseaes.2023.105773
英文摘要The formation of Fe-Ti oxide ore bodies in layered intrusions is attributed to in situ crystallization of basaltic magmas or accumulation after crystal settling regardless of their thicknesses and occurrences in the intrusion. These two key processes are difficult to be distinguished in terms of chemical compositions of minerals or cumulates. However, the crystal size distributions (CSDs) of Fe-Ti oxides in the rocks can be remarkably distinct in these two processes. In this study, we collected samples from a drill core profile across the major Fe-Ti oxide-rich segment of the Bijigou intrusion, a large and differentiated layered intrusion in Central China, and carried out a detailed study on the CSDs and in situ major and trace elements of magnetite and ilmenite to examine how Fe-Ti oxides are accumulated to form Fe-Ti oxide ore bodies in the intrusion. The major Fe-Ti oxide-rich segment of the intrusion consists of, from the base upward, a Fe-Ti oxide ore layer (-80 m), a troctolite unit (-105 m), an oxide gabbro unit (-153 m) and an apatite-oxide gabbronorite unit (-165 m). Large grains of magnetite and ilmenite in the Fe-Ti oxide ore layer show logarithmic-linear CSD curves, similar to those yielded by in situ crystallization of Fe-Ti oxides. The modes of Fe-Ti oxides in the oxide gabbro unit and apatite-oxide gabbronorite unit fluctuate along the profile, which cannot be attributed to accumulation after crystal settling. In addition, the magnetite of the Fe-Ti oxide ore layer, oxide gabbro unit and apatite-oxide gabbronorite unit shows a gentle increase trend of Cr concentration from the base upward in each unit, inconsistent with the trend for an accumulation after crystal settling. The magnetite grains enclosed within silicates have similar compositions to those interstitial to silicates, indicating that they all crystallized from similarly interstitial Fe-rich melt. The in situ crystallization of Fe-Ti oxides is likely triggered by increasing oxygen fugacity due to dissociation of H2O in highly evolved interstitial liquid that was expelled from underlying crystal mush. The crystallization of low-Cr magnetite at the base of each unit is attributed to suppressed eddy currents by dramatic increase of latent heat of crystallization in the magmas at the base. The eddy currents may gradually become efficient toward the top of the magmas due to rapid dissipation of latent heat of crystallization in the magmas, leading to crystallization of high-Cr magnetite by ion diffusion on the top of each unit. This study also demonstrates that analysis of CSDs for Fe-Ti oxides is applicable to examine the accumulation mechanism of Fe-Ti oxide ore bodies in layered intrusions.
WOS研究方向Geology
语种英语
WOS记录号WOS:001036292600001
源URL[http://ir.gig.ac.cn/handle/344008/74568]  
专题中国科学院矿物学与成矿学重点实验室
通讯作者Wang, Mengxi
作者单位1.Changan Univ, Sch Earth Sci & Resources, Xian 710054, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.Guangzhou Inst Geochem, CAS Key Lab Mineral & Metallogeny, Guangzhou 510640, Peoples R China
推荐引用方式
GB/T 7714
Wang, Mengxi,Zhang, Buqian,Li, Zhongzhou,et al. In situ crystallization of Fe-Ti oxides in the Bijigou layered intrusion: Insights from crystal size distributions and compositions of magnetite and ilmenite[J]. JOURNAL OF ASIAN EARTH SCIENCES,2023,255:17.
APA Wang, Mengxi,Zhang, Buqian,Li, Zhongzhou,Wang, Jie,&Wang, Jiangze.(2023).In situ crystallization of Fe-Ti oxides in the Bijigou layered intrusion: Insights from crystal size distributions and compositions of magnetite and ilmenite.JOURNAL OF ASIAN EARTH SCIENCES,255,17.
MLA Wang, Mengxi,et al."In situ crystallization of Fe-Ti oxides in the Bijigou layered intrusion: Insights from crystal size distributions and compositions of magnetite and ilmenite".JOURNAL OF ASIAN EARTH SCIENCES 255(2023):17.

入库方式: OAI收割

来源:广州地球化学研究所

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