Gas discharges from the Kueishantao hydrothermal vents, offshore northeast Taiwan: Implications for drastic variations of magmatic/hydrothermal activities
文献类型:期刊论文
作者 | Chen, Yun-Jie3,5; Chen, Xue-Gang3; Li, Xiaohu6; Jin, Aimin3; Zhang, Hai-Yan4![]() |
刊名 | JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH
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出版日期 | 2018-03-15 |
卷号 | 353页码:1-10 |
关键词 | Kueishantao Model Hydrothermal Vent Hydrocarbon Co2 Magmatic Activity |
DOI | 10.1016/j.jvolgeores.2018.01.013 |
产权排序 | 第1完成单位 ; 第2完成单位 ; 第3完成单位 ; 第4完成单位 ; 第5完成单位 ; 第6完成单位 |
文献子类 | Article |
英文摘要 | The chemical compositions of gas discharges from the Kueishantao (KST) hydrothermal field changed dramatically from 2000 to 2014. In this study, we established a gas mixing model for the KST gases. The N-2, Ar, and CO2 contents were mixed from a magmatic endmember with CO2 of about 990 mmol/mol, a hydrothermal and an atmospheric endmember enriched in N-2 and Ar. More than 71% KST gas components were mantle-derived/magmatic The calculated endmember N-2/Ar ratio and Ar contents of the hydrothermal endmember (percolated fluid) are about 140 and 5.28-5.52 mmol/mol, respectively. This relatively elevated N-2/Ar ratio was probably caused by the thermogenic addition of N-2. The log(CH4/CO2) values of the KST gas samples correlate well with the mixing temperature that estimated from the mixing ratio between the percolated fluid and the magmatic endmember. It is indicated that the KST CH4 and CO2 may have attained chemical equilibrium. The temporal variations of the KST gas compositions are determined by the mixing ratio, which is dependent on the magmatic activity underneath the KST field. With the decreasing of magmatic activity since 2005, the proportion of the hydrothermal endmember increased, along with the increasing of N-2, Ar, and CH4 contents. This study proposed an effective model to quantitatively assess the sources of gas components discharged from submarine hydrothermal vents. In addition, it is suggested that the mixing between a magmatic and a hydrothermal endmember may play an important role in the concentrations of CO2 and CH4 in hydrothermal gas discharges. (C) 2017 Elsevier B.V. All rights reserved. |
URL标识 | 查看原文 |
WOS关键词 | HYDROGEN ISOTOPE SYSTEMATICS ; MID-ATLANTIC RIDGE ; ABIOTIC METHANE ; FUMAROLIC GAS ; RAPID CHANGES ; ORIGIN ; FLUIDS ; CARBON ; HYDROCARBONS ; RATIOS |
语种 | 英语 |
WOS记录号 | WOS:000429184300001 |
源URL | [http://ir.idsse.ac.cn/handle/183446/5934] ![]() |
专题 | 深海科学研究部_深海极端环境模拟研究实验室 |
通讯作者 | Duan, Wei; Duan, Wei(Zhejiang Univ, Ocean Coll, Zhoushan 316021, Peoples R China) |
作者单位 | 1.Natl Sun Yat Sen Univ, Dept Oceanog, Kaohsiung 80424, Taiwan 2.Zhejiang Inst Geol & Mineral Resources, Hangzhou 310007, Zhejiang, Peoples R China 3.Zhejiang Univ, Ocean Coll, Zhoushan 316021, Peoples R China 4.Chinese Acad Sci, Inst Deep Sea Sci & Engn, Sanyo 572000, Peoples R China 5.Univ Aberdeen, Dept Geol & Petr Geol, Aberdeen AB24 3UE, Scotland 6.State Ocean Adm, Key Lab Submarine Geosci, Hangzhou 310012, Zhejiang, Peoples R China |
推荐引用方式 GB/T 7714 | Chen, Yun-Jie,Chen, Xue-Gang,Li, Xiaohu,et al. Gas discharges from the Kueishantao hydrothermal vents, offshore northeast Taiwan: Implications for drastic variations of magmatic/hydrothermal activities[J]. JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH,2018,353:1-10. |
APA | Chen, Yun-Jie.,Chen, Xue-Gang.,Li, Xiaohu.,Jin, Aimin.,Zhang, Hai-Yan.,...&Lyu, Shuang-Shuang.(2018).Gas discharges from the Kueishantao hydrothermal vents, offshore northeast Taiwan: Implications for drastic variations of magmatic/hydrothermal activities.JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH,353,1-10. |
MLA | Chen, Yun-Jie,et al."Gas discharges from the Kueishantao hydrothermal vents, offshore northeast Taiwan: Implications for drastic variations of magmatic/hydrothermal activities".JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH 353(2018):1-10. |
入库方式: OAI收割
来源:深海科学与工程研究所
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