Volatile element isotopes of submarine hydrothermal mineral deposits in the Western Pacific
文献类型：期刊论文
| 作者 | Ooki, Mitsuhiro1,2; Kagoshima, Takanori1; Takahata, Naoto1; Ishibashi, Jun-ichiro3; Lan, Tefang4; Guo, Zhengfu5; Sano, Yuji1,6 |
| 刊名 | GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
 |
| 出版日期 | 2016-06-01 |
| 卷号 | 17期号:6页码:2128-2142 |
| 关键词 | hydrothermal mineral deposits subduction zones noble gas stable isotopes marine sediment |
| DOI | 10.1002/2016GC006360 |
| 文献子类 | Article |
| 英文摘要 | The abundance and isotopic compositions of volatile elements trapped in fluid inclusions of submarine hydrothermal mineral deposits in Western Pacific subduction zones (Okinawa Trough, Izu-Bonin arc, Mariana Trough, and Lau Basin) and in Kuroko ores in northeastern Japan are presented. The helium isotopic compositions corrected for air contribution of the Okinawa and Mariana troughs, ranging 4.49-7.68 Ra are lower than those of the Izu-Bonin and Lau Basin, 7.62-8.91 Ra. This characteristic might reflect the differences in regional tectonic setting. The Okinawa and Mariana troughs are related to back-arc spreading with strong graben sedimentary signature, whereas the Izu-Bonin arc is associated with island arc magmatism. The arc contribution to the Lau Basin volcanism is significantly strong, even though it is assigned to back-arc spreading. Nitrogen isotopes can also be explained by a similar hypothesis, whereas argon and carbon isotopes cannot be used to discriminate tectonic setting. C-13-CO2/He-3 and N-15-N-2/Ar-36 diagrams elucidate the source of carbon and nitrogen. The MOR-type mantle contributions to carbon are mostly smaller in the Okinawa and Mariana troughs (ranging 0.06-8.9% with the average of 2.4%) than in the Izu-Bonin and Lau Basin (2.1-25% with the average of 7.7%). The sedimentary contributions to nitrogen are larger in the Okinawa and Mariana troughs (11-65% with the average of 35%) than in the Izu-Bonin and Lau Basin (4-24% with the average of 15%), and the Kuroko samples agree well with the latter. Carbon and nitrogen fluxes are again higher in Okinawa trough than in Izu-Bonin arc. |
| WOS关键词 | MID-OKINAWA TROUGH ; BACK-ARC BASIN ; HELIUM ISOTOPE ; ATMOSPHERIC HELIUM ; CONTINENTAL-CRUST ; MIDOCEAN RIDGE ; CHEMICAL-COMPOSITION ; SUBDUCTION ZONES ; KUROKO DEPOSITS ; OCEANIC BASALTS |
| WOS研究方向 | Geochemistry & Geophysics |
| 语种 | 英语 |
| WOS记录号 | WOS:000380728300010 |
| 资助机构 | MEXT, Japan(15H05830) ; MEXT, Japan(15H05830) ; MEXT, Japan(15H05830) ; MEXT, Japan(15H05830) |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/53379]  |
| 专题 | 地质与地球物理研究所_中国科学院新生代地质与环境重点实验室 |
| 作者单位 | 1.Univ Tokyo, Atmosphere & Ocean Res Inst, Kashiwa, Chiba, Japan 2.Mitsui Min & Smelting Co Ltd, Tokyo, Japan 3.Kyushu Univ, Dept Earth & Planetary Sci, Fac Sci, Fukuoka, Japan 4.Acad Sinica, Inst Earth Sci, Taipei, Taiwan 5.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing, Peoples R China 6.Natl Taiwan Univ, Dept Geosci, Taipei, Taiwan |
| 推荐引用方式 GB/T 7714 | Ooki, Mitsuhiro,Kagoshima, Takanori,Takahata, Naoto,et al. Volatile element isotopes of submarine hydrothermal mineral deposits in the Western Pacific[J]. GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS,2016,17(6):2128-2142. |
| APA | Ooki, Mitsuhiro.,Kagoshima, Takanori.,Takahata, Naoto.,Ishibashi, Jun-ichiro.,Lan, Tefang.,...&Sano, Yuji.(2016).Volatile element isotopes of submarine hydrothermal mineral deposits in the Western Pacific.GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS,17(6),2128-2142. |
| MLA | Ooki, Mitsuhiro,et al."Volatile element isotopes of submarine hydrothermal mineral deposits in the Western Pacific".GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS 17.6(2016):2128-2142. |
入库方式： OAI收割
来源：地质与地球物理研究所
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