Geochemical and Sr-Nd-Pb isotopic compositions of volcanic rocks from the Iheya Ridge, the middle Okinawa Trough: implications for petrogenesis and a mantle source
文献类型：期刊论文
| 作者 | Li, Xiaohui1,2; Zeng, Zhigang1,3; Chen, Shuai1; Ma, Yao1 ; Yang, Huixin1; Zhang, Yuxiang1,2; Chen, Zuxing1,2
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| 刊名 | ACTA OCEANOLOGICA SINICA
 |
| 出版日期 | 2018 |
| 卷号 | 37期号:1页码:73-88 |
| 关键词 | Basic To Intermediate-acid Rocks Fractional Crystallization Subduction Sediment Components Iheya Ridge Okinawa Trough |
| DOI | 10.1007/s13131-017-1118-8 |
| 文献子类 | Article |
| 英文摘要 | As an active back-arc basin, the Okinawa Trough is located in the southeastern region of the East China Sea shelf and is strongly influenced by the subduction of the Philippine Sea Plate. Major element, trace element and Sr-Nd- Pb isotopic composition data are presented for volcanic rocks from the Iheya Ridge (IR), the middle Okinawa Trough. The IR rocks record large variations in major elements and range from basalts to rhyolites. Similar trace element distribution characteristics together with small variations in Sr-87/Sr-86 (0.703 862-0.704 884), Nd-144/Nd-143 (0.512 763-0.512 880) and Pb isotopic ratios, demonstrate that the IR rocks are derived from a similar magma source. The fractional crystallization of olivine, clinopyroxene, plagioclase, and amphibole, as well as accessory minerals, can reasonably explain the compositional variations of these IR rocks. The simulations suggest that approximately 60% and 75% fractionation of an evolved basaltic magma can produce trace element compositions similar to those of the intermediate rocks and acid rocks, respectively. The analysis of their Sr-Nd-Pb isotopic content ratios suggest that the source of the rocks from the IR is close to the depleted mantle (DM) but extends to the enriched mantle (EMII), indicating that the mantle source of these rocks is a mixture between the DM and EMII end members. The simulations show that the source of the IR volcanic rocks can be best interpreted as the result of the mixing of approximately 0.8%-2.0% subduction sediment components and 98.0%-99.2% mantlederived melts. |
| 语种 | 英语 |
| WOS记录号 | WOS:000419193900008 |
| 版本 | 出版稿 |
| 源URL | [http://ir.qdio.ac.cn/handle/337002/154326]  |
| 专题 | 海洋研究所_海洋地质与环境重点实验室 |
| 作者单位 | 1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China 2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 3.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Mineral Resources, Qingdao 266071, Peoples R China |
| 推荐引用方式 GB/T 7714 | Li, Xiaohui,Zeng, Zhigang,Chen, Shuai,et al. Geochemical and Sr-Nd-Pb isotopic compositions of volcanic rocks from the Iheya Ridge, the middle Okinawa Trough: implications for petrogenesis and a mantle source[J]. ACTA OCEANOLOGICA SINICA,2018,37(1):73-88. |
| APA | Li, Xiaohui.,Zeng, Zhigang.,Chen, Shuai.,Ma, Yao.,Yang, Huixin.,...&Chen, Zuxing.(2018).Geochemical and Sr-Nd-Pb isotopic compositions of volcanic rocks from the Iheya Ridge, the middle Okinawa Trough: implications for petrogenesis and a mantle source.ACTA OCEANOLOGICA SINICA,37(1),73-88. |
| MLA | Li, Xiaohui,et al."Geochemical and Sr-Nd-Pb isotopic compositions of volcanic rocks from the Iheya Ridge, the middle Okinawa Trough: implications for petrogenesis and a mantle source".ACTA OCEANOLOGICA SINICA 37.1(2018):73-88. |
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来源：海洋研究所
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