The oxidized granitoids facilitated the formation of Early Cretaceous molybdenum mineralization in the Jiaodong region, China
文献类型：期刊论文
| 作者 | Yan, Maoqiang5; Li, Jie1,5 ; Zhang, Lipeng5; Sun, Weidong2,3,5; Li, Congying4,5
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| 刊名 | ORE GEOLOGY REVIEWS
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| 出版日期 | 2024-03-01 |
| 卷号 | 166页码:14 |
| 关键词 | Porphyry Mo deposit Magma oxygen fugacity Zircon trace elements Hf -O isotope Mesozoic magmatism |
| ISSN号 | 0169-1368 |
| DOI | 10.1016/j.oregeorev.2024.105931 |
| 通讯作者 | Li, Congying(licongying@qdio.ac.cn) |
| 英文摘要 | Oxygen fugacity is a key factor in controlling the formation of porphyry molybdenum deposits. We present new data on Lengjia monzogranite and compile the Mesozoic magmatism data of the Jiaodong Peninsula to elucidate the correlation between magma oxygen fugacity and porphyry Mo mineralization. Zircon U -Pb geochronology indicates that the formation of the Lengjia monzogranite occurred at 113.7 Ma, while molybdenite Re -Os geochronology shows that the Lengjia Mo deposit was formed at 113.5 +/- 3.0 Ma. The Lengjia monzogranite, characterized by low Sr/Y ratios (12.28 - 20.16), low Sr, and high Yb and Y concentrations, can be classified as a non-adakite I -type granite. It had low zircon epsilon Hf (t) values (-23.8 - -13.8) and ancient TDM2 (Hf) (2047-2680 Ma) with variable zircon O isotopic compositions (5.82 %o - 7.38 %o). The Lengjia monzogranite was formed by partial melting of the Paleoproterozoic crustal source and mantle components metasomatized by slab-derived melt. The zircon trace element calculation revealed that the Weideshan suite had higher Delta FMQ values (0.32 - 4.47, average is 2.27) compared to the Guojialing suite (-0.91 - 2.88, average is 0.82) and Linglong suite (-1.81 - 2.76, average is 0.37). The oxidized Weideshan suite resulted from the increased involvement of mantle metasomatized by slab-derived melt. The elevated oxygen fugacity promoted the porphyry Mo-metallogenic potential of the Weidshanian suite. We propose that the Linglong suite was related to the northwestward flatslab (subhorizontal) subduction of the Izanagi plate (Paleo-Pacific plate), the Guojialing suite was formed by low-angle northwestward subduction of the Izanagi plate, and the Weideshan suite was related to the northwestward subduction and major slab rollback of the Pacific plate. |
| WOS关键词 | PORPHYRY MO DEPOSITS ; YANGTZE-RIVER BELT ; HF-O ISOTOPES ; ZIRCON U-PB ; OXIDATION-STATE ; EASTERN CHINA ; TRACE-ELEMENT ; CU DEPOSITS ; GOLD MINERALIZATION ; NORTHEASTERN CHINA |
| 资助项目 | National Natural Science Founda- tion of China[42176070] ; Youth Innovation Promotion Association of Chinese Academy of Sciences[2020212] ; Laoshan Laboratory[LSKJ202204100] |
| WOS研究方向 | Geology ; Mineralogy ; Mining & Mineral Processing |
| 语种 | 英语 |
| WOS记录号 | WOS:001188148900001 |
| 出版者 | ELSEVIER |
| 源URL | [http://ir.qdio.ac.cn/handle/337002/184941]  |
| 专题 | 海洋研究所_深海极端环境与生命过程研究中心 |
| 通讯作者 | Li, Congying |
| 作者单位 | 1.Hebei GEO Univ, Hebei Key Lab Strateg Crit Mineral Resources, Shijiazhuang, Peoples R China 2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 3.Laoshan Lab, Deep Sea Multidisciplinary Res Ctr, Qingdao 266237, Peoples R China 4.Lab Marine Mineral Resources, Laoshan Lab, Qingdao 266237, Peoples R China 5.Chinese Acad Sci, Inst Oceanol, Ctr Deep Sea Res, Qingdao 266071, Peoples R China |
| 推荐引用方式 GB/T 7714 | Yan, Maoqiang,Li, Jie,Zhang, Lipeng,et al. The oxidized granitoids facilitated the formation of Early Cretaceous molybdenum mineralization in the Jiaodong region, China[J]. ORE GEOLOGY REVIEWS,2024,166:14. |
| APA | Yan, Maoqiang,Li, Jie,Zhang, Lipeng,Sun, Weidong,&Li, Congying.(2024).The oxidized granitoids facilitated the formation of Early Cretaceous molybdenum mineralization in the Jiaodong region, China.ORE GEOLOGY REVIEWS,166,14. |
| MLA | Yan, Maoqiang,et al."The oxidized granitoids facilitated the formation of Early Cretaceous molybdenum mineralization in the Jiaodong region, China".ORE GEOLOGY REVIEWS 166(2024):14. |
入库方式： OAI收割
来源：海洋研究所
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