Mineralogy and Geochemistry of Titaniferous Iron Ores in El-Baroud Layered Gabbros: Fe-Ti Ore Genesis and Tectono-Metallogenetic Setting
文献类型：期刊论文
| 作者 | Khedr, Mohamed Zaki3; Moftah, Ahmed3; El-Shibiny, N. H.3; Tamura, Akihiro4; Tan, Wei5; Ichiyama, Yuji1; Takazawa, Eiichi6; Kahal, Ali Y.2; Abdelrahman, Kamal2 |
| 刊名 | MINERALS
 |
| 出版日期 | 2024-07-01 |
| 卷号 | 14期号:7页码:38 |
| 关键词 | gabbroic intrusion Fe-Ti oxide ores mineral chemistry liquid immiscibility arc rifting Arabian-Nubian Shield |
| DOI | 10.3390/min14070679 |
| 英文摘要 | The Neoproterozoic pyroxene gabbros and gabbronorites in the El-Baroud mafic intrusion in the Northern Eastern Desert (NED) of Egypt host Fe-Ti oxide ore deposits. This study discusses the major and trace elements of both titaniferous iron ores and their host rocks, along with the mineral chemistry (major and in situ trace elements) of interstitial clinopyroxene (Cpx), to gain a deeper understanding of the Fe-Ti oxide genesis. These ores occur as disseminated (55-60 vol.% of Fe-Ti oxides) and massive types (85-95 vol.%) in the form of the dyke, layer, and lens. They are composed of titanomagnetite (80-87 vol.%) with subordinate ilmenite (10-15 vol.%) and magnetite (3-5 vol.%), in accordance with their high Fe2O3 (75.66 wt.% on average) and TiO2 contents (16.30-17.60 wt.%). The Cpx in the investigated ores is diopside composition (Mg#; 0.72-0.83) and exhibits a nearly convex upward REE pattern, similar to Cpxs in the ferropicrite that originated from the primitive mantle. Melts in equilibrium with this Cpx resemble Greenstone ferropicrite melts; the parent melt of El-Baroud gabbros is possibly a ferropicritic melt that was derived from the lithospheric mantle during plume interaction. The El-Baroud gabbroic rocks were generated during the arc rifting and crystallized under a high oxygen fugacity at a temperature of 800-1000 degrees C and a pressure of 3 kbar with a depth of 12 km. The Fe-Ti oxide ores have been formed from ferropicritic parent melts by two processes, including in situ crystallization that leads to the formation of disseminated Fe-Ti oxides in the iron-rich gabbros at the bottom and liquid immiscibility that is responsible for the formation of thick Fe-Ti ore lenses and layers at the top of the gabbroic intrusion. Initially, titanomagnetite crystallized from the primary Ti-rich oxide melt. As cooling progressed, some of the excess titanium in this melt was exsolved in the form of the exsolution ilmenite lamellae within the titanomagnetite. The Fe-Ti oxide layers in the NED follow the trend of NW-SE (Najd trend), where their distribution is possibly controlled by the composition of parent melts (rich in Ti and Fe), high oxygen fugacity, and the structure related to the Najd fault system. The distribution of Fe-Ti oxide ores increases from the NED to the Southern Eastern Desert (SED), suggesting the dominant mantle plumes and/or shear zones in the SED relative to the NED. |
| WOS研究方向 | Geochemistry & Geophysics ; Mineralogy ; Mining & Mineral Processing |
| 语种 | 英语 |
| WOS记录号 | WOS:001277427600001 |
| 源URL | [http://ir.gig.ac.cn/handle/344008/78195]  |
| 专题 | 中国科学院矿物学与成矿学重点实验室 |
| 通讯作者 | Khedr, Mohamed Zaki |
| 作者单位 | 1.Chiba Univ, Grad Sch Sci, 1-33 Yayoi Cho,Inage Ku, Chiba 2638522, Japan 2.King Saud Univ, Coll Sci, Dept Geol & Geophys, POB 2455, Riyadh 11451, Saudi Arabia 3.Kafrelsheikh Univ, Fac Sci, Dept Geol, Kafrelsheikh 33516, Egypt 4.Kanazawa Univ, Dept Earth Sci, Kanazawa, Ishikawa 9201192, Japan 5.Chinese Acad Sci, Guangzhou Inst Geochem, Key Lab Mineral & Metallogeny, Guangzhou 510640, Peoples R China 6.Niigata Univ, Fac Sci, Geol Dept, Niigata 9502181, Japan |
| 推荐引用方式 GB/T 7714 | Khedr, Mohamed Zaki,Moftah, Ahmed,El-Shibiny, N. H.,et al. Mineralogy and Geochemistry of Titaniferous Iron Ores in El-Baroud Layered Gabbros: Fe-Ti Ore Genesis and Tectono-Metallogenetic Setting[J]. MINERALS,2024,14(7):38. |
| APA | Khedr, Mohamed Zaki.,Moftah, Ahmed.,El-Shibiny, N. H..,Tamura, Akihiro.,Tan, Wei.,...&Abdelrahman, Kamal.(2024).Mineralogy and Geochemistry of Titaniferous Iron Ores in El-Baroud Layered Gabbros: Fe-Ti Ore Genesis and Tectono-Metallogenetic Setting.MINERALS,14(7),38. |
| MLA | Khedr, Mohamed Zaki,et al."Mineralogy and Geochemistry of Titaniferous Iron Ores in El-Baroud Layered Gabbros: Fe-Ti Ore Genesis and Tectono-Metallogenetic Setting".MINERALS 14.7(2024):38. |
入库方式： OAI收割
来源：广州地球化学研究所
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