Molybdenum isotopic fractionation in the Panzhihua mafic layered intrusion in the Emeishan large igneous province, southwest China
文献类型：期刊论文
| 作者 | Zhang, Le2,3; Li, Jie2,3 ; Zhang, Yan1; Peng, Bing-Yu2,3; Wang, Zhi-Bing2,3; Ren, Zhong-Yuan2,3
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| 刊名 | AMERICAN MINERALOGIST
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| 出版日期 | 2024-03-25 |
| 卷号 | 109期号:3页码:628-632 |
| 关键词 | Mo isotope fractionation magmatic differentiation Panzhihua intrusion Emeishan large igneous province Isotopes, Minerals, and Petrology Honoring John Valley |
| ISSN号 | 0003-004X |
| DOI | 10.2138/am-2023-9154 |
| 英文摘要 | The large Mo isotopic fractionations between diferent geological reservoirs make this isotopic system a potentially useful tool for constraining the origins of magmatism. However, the efect of magmatic diferentiation on Mo isotopes is still controversial. In this study, we obtained Mo isotope data for the Panzhihua gabbroic intrusion (i.e., including mineral separates of clinopyroxene, plagioclase, magnetite, and ilmenite). The whole-rock samples and mineral separates exhibit large Mo isotopic fractionations with delta Mo-98/95 values as follows: magnetite (-0.73 parts per thousand to -0.32 parts per thousand ) < clinopyroxene (-0.32 parts per thousand to -0.10 parts per thousand ) < ilmenite (0.06 parts per thousand to 0.36 parts per thousand ) < plagioclase (0.33 parts per thousand to 0.83 parts per thousand ). Iron-Ti oxides have Mo contents that are one order of magnitude higher than those of clinopyroxene and plagioclase. Mass balance calculations based on Mo isotopes and contents are consistent with an accumulated origin for the Panzhihua intrusion. Rayleigh fractionation modeling shows that the removal of magnetite and ilmenite results in significant Mo isotopic fractionation in the residual magma. Due to the low Mo contents of clinopyroxene and plagioclase, Mo isotopes are not significantly fractionated by the removal of these minerals. Therefore, our study highlights that fractionation of Fe-Ti oxides can cause considerable Mo isotopic fractionation; consequently, caution is needed when using Mo isotopes to infer magma origins. |
| WOS研究方向 | Geochemistry & Geophysics ; Mineralogy |
| 语种 | 英语 |
| WOS记录号 | WOS:001183294700020 |
| 源URL | [http://ir.gig.ac.cn/handle/344008/77136]  |
| 专题 | 同位素地球化学国家重点实验室 |
| 通讯作者 | Zhang, Le |
| 作者单位 | 1.Minist Nat Resources, Inst Oceanog 1, Key Lab Marine Geol & Metallogeny, Qingdao 266061, Peoples R China 2.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510640, Peoples R China 3.CAS Ctr Excellence Deep Earth Sci, Guangzhou 510640, Peoples R China |
| 推荐引用方式 GB/T 7714 | Zhang, Le,Li, Jie,Zhang, Yan,et al. Molybdenum isotopic fractionation in the Panzhihua mafic layered intrusion in the Emeishan large igneous province, southwest China[J]. AMERICAN MINERALOGIST,2024,109(3):628-632. |
| APA | Zhang, Le,Li, Jie,Zhang, Yan,Peng, Bing-Yu,Wang, Zhi-Bing,&Ren, Zhong-Yuan.(2024).Molybdenum isotopic fractionation in the Panzhihua mafic layered intrusion in the Emeishan large igneous province, southwest China.AMERICAN MINERALOGIST,109(3),628-632. |
| MLA | Zhang, Le,et al."Molybdenum isotopic fractionation in the Panzhihua mafic layered intrusion in the Emeishan large igneous province, southwest China".AMERICAN MINERALOGIST 109.3(2024):628-632. |
入库方式： OAI收割
来源：广州地球化学研究所
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