Origin of Cu in the PACMANUS hydrothermal field from the eastern Manus back-arc basin: evidence from mass balance modeling | |
Ma, Yao3,4; Wang, Xiaoyuan3,4; Chen, Shuai3,4; Yin, Xuebo4; Zhu, Bowen2,4; Guo, Kun1,3,4; Zeng, Zhigang2,3,4 | |
刊名 | ACTA OCEANOLOGICA SINICA |
2019-09-01 | |
卷号 | 38期号:9页码:59-70 |
关键词 | back-arc basin mass balance model PACMANUS hydrothermal field source of Cu |
ISSN号 | 0253-505X |
DOI | 10.1007/s13131-019-1475-z |
通讯作者 | Ma, Yao(mayao@qdio.ac.cn) |
英文摘要 | Hydrothermal precipitates associated with active vents in the eastern Manus Basin, an actively opening back-arc basin in the Bismarck Sea, Papua New Guinea, are among the most Cu-rich on the modern seafloor. The volcanic rocks associated with this mineralization may be insufficiently enriched in Cu to account for the Cu content of the sulfides by simple leaching. The PACMANUS hydrothermal field lies in the eastern portion of the eastern Manus Basin. Mass balance modeling of the PACMANUS hydrothermal system indicates that simple leaching of a stationary reaction zone (0.144 km(3)) by hydrothermal fluids cannot yield the Cu found in associated sulfide deposits because unacceptably high leaching, transportation and precipitation efficiencies are required to derive the Cu in sulfides by leaching processes. With 100% leaching, transport and precipitating efficiency, 0.166 km(3) of volcanic rocks would need to be leached to account for the Cu budget of hydrothermal sulfide deposits. The key requirement for forming metal-rich magmatic fluids is a large amount of metals available to enter the exsolved vapor phase. Magmas generated in the eastern Manus Basin inherently have high fO(2) because of metasomatism of the mantle source by oxidized materials from the subducted slab, leading to copper enrichment in the magma chamber. Moreover, the presence of Cu in gas-rich melt inclusi on bubbles in Pual Ridge andesite is evidence that degassing and partitioning of Cu into the magmatic volatile phase has occurred in the eastern Manus Basin. Numerical mass balance modeling indicates that approximately 0.236 Mt Cu was potentially transferred to the hydrothermal system per cubic kilometer magma. Magmatic degassing seems to play a more significant role than leaching. |
资助项目 | National Natural Science Foundation of China[41706052] ; National Natural Science Foundation of China[41476044] ; National Natural Science Foundation of China[41325021] ; National Program on Global Change and Air-Sea Interaction[GASI-GEOGE-02] ; National Basic Research Program (973 Program) of China[2013CB429700] ; International Partnership Program of Chinese Academy of Sciences[133137KYSB20170003] ; Strategic Priority Research Program of the Chinese Academy of Sciences[XDA11030302] ; Special Fund for the Taishan Scholar Program of Shandong Province[ts201511061] ; National Special Fund for the 13th Five Year Plan of COMRA[DY135-G2-1-02] ; AoShan Talents Program - Qingdao National Laboratory for Marine Science and Technology[2015ASTP-0S17] ; Innovative Talent Promotion Program[2012RA2191] ; Science and Technology Development Program of Shandong Province[2013GRC31502] ; Scientific and Technological Innovation Project - Qingdao National Laboratory for Marine Science and Technology[2015ASKJ03] ; National High Level Talent Special Support Program ; CAS/SAFEA International Partnership Program for Creative Research Teams ; Qingdao Collaborative Innovation Center of Marine Science and Technology |
WOS研究方向 | Oceanography |
语种 | 英语 |
出版者 | SPRINGER |
WOS记录号 | WOS:000485996200006 |
内容类型 | 期刊论文 |
源URL | [http://ir.qdio.ac.cn/handle/337002/162989] |
专题 | 海洋研究所_海洋地质与环境重点实验室 |
通讯作者 | Ma, Yao |
作者单位 | 1.Pilot Natl Lab Marine Sci & Technol, Ocean Sci Isotope & Geochronol Ctr, Qingdao 266071, Shandong, Peoples R China 2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 3.Pilot Natl Lab Marine Sci & Technol Qingdao, Lab Marine Mineral Resources, Qingdao 266071, Shandong, Peoples R China 4.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Shandong, Peoples R China |
推荐引用方式 GB/T 7714 | Ma, Yao,Wang, Xiaoyuan,Chen, Shuai,et al. Origin of Cu in the PACMANUS hydrothermal field from the eastern Manus back-arc basin: evidence from mass balance modeling[J]. ACTA OCEANOLOGICA SINICA,2019,38(9):59-70. |
APA | Ma, Yao.,Wang, Xiaoyuan.,Chen, Shuai.,Yin, Xuebo.,Zhu, Bowen.,...&Zeng, Zhigang.(2019).Origin of Cu in the PACMANUS hydrothermal field from the eastern Manus back-arc basin: evidence from mass balance modeling.ACTA OCEANOLOGICA SINICA,38(9),59-70. |
MLA | Ma, Yao,et al."Origin of Cu in the PACMANUS hydrothermal field from the eastern Manus back-arc basin: evidence from mass balance modeling".ACTA OCEANOLOGICA SINICA 38.9(2019):59-70. |
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