中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Origin of methane-rich natural gas at the West Pacific convergent plate boundary

文献类型:期刊论文

作者Sano, Yuji1; Kinoshita, Naoya1; Kagoshima, Takanori1; Takahata, Naoto1; Sakata, Susumu2; Toki, Tomohiro3; Kawagucci, Shinsuke4; Waseda, Amane5; Lan, Tefang6; Wen, Hsinyi6,7
刊名SCIENTIFIC REPORTS
出版日期2017-11-15
卷号7
ISSN号2045-2322
DOI10.1038/s41598-017-15959-5
文献子类Article
英文摘要Methane emission from the geosphere is generally characterized by a radiocarbon-free signature and might preserve information on the deep carbon cycle on Earth. Here we report a clear relationship between the origin of methane-rich natural gases and the geodynamic setting of the West Pacific convergent plate boundary. Natural gases in the frontal arc basin (South Kanto gas fields, Northeast Japan) show a typical microbial signature with light carbon isotopes, high CH4/C2H6 and CH4/He-3 ratios. In the Akita-Niigata region-which corresponds to the slope stretching from the volcanic-arc to the back-arc-a thermogenic signature characterize the gases, with prevalence of heavy carbon isotopes, low CH4/C2H6 and CH4/He-3 ratios. Natural gases from mud volcanoes in South Taiwan at the collision zone show heavy carbon isotopes, middle CH4/C2H6 ratios and low CH4/He-3 ratios. On the other hand, those from the Tokara Islan(d)s situated on the volcanic front of Southwest Japan show the heaviest carbon isotopes, middle CH4/C2H6 ratios and the lowest CH4/He-3 ratios. The observed geochemical signatures of natural gases are clearly explained by a mixing of microbial, thermogenic and abiotic methane. An increasing contribution of abiotic methane towards more tectonically active regions of the plate boundary is suggested.
WOS关键词ISOTOPIC COMPOSITION ; SW TAIWAN ; GEOGRAPHICAL-DISTRIBUTION ; HYDROTHERMAL FLUIDS ; MOLECULAR NITROGEN ; HE-3/HE-4 RATIOS ; MUD VOLCANOS ; NOBLE-GASES ; CRUDE OILS ; CARBON
WOS研究方向Science & Technology - Other Topics
语种英语
WOS记录号WOS:000415265800057
出版者NATURE PUBLISHING GROUP
资助机构MEXT, Japan(15H05830 ; 17H00777) ; MEXT, Japan(15H05830 ; 17H00777) ; MEXT, Japan(15H05830 ; 17H00777) ; MEXT, Japan(15H05830 ; 17H00777)
源URL[http://ir.iggcas.ac.cn/handle/132A11/62436]  
专题地质与地球物理研究所_兰州油气中心
通讯作者Sano, Yuji
作者单位1.Univ Tokyo, Atmosphere & Ocean Res Inst, Kashiwa, Chiba, Japan
2.Natl Inst Adv Ind Sci & Technol, Inst Georesources & Environm, Tsukuba, Ibaraki, Japan
3.Univ Ryukyus, Dept Chem Biol & Marine Sci, Okinawa, Japan
4.Japan Agcy Marine Earth Sci & Technol, Dept Subsurface Geobiol Anal & Res, Yokosuka, Kanagawa, Japan
5.Japan Petr Explorat Co Ltd, Tokyo, Japan
6.Natl Taiwan Univ, Dept Geosci, Taipei, Taiwan
7.Ind Technol Res Inst, Green Energy & Environm Res Labs, Hsinchu, Taiwan
8.Acad Sinica, Inst Earth Sci, Taipei, Taiwan
9.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Petr Resources, Gansu Prov Key Lab Petr Resources Res, Lanzhou 730000, Gansu, Peoples R China
10.Univ Bern, Inst Geol Sci, Bern, Switzerland
推荐引用方式
GB/T 7714
Sano, Yuji,Kinoshita, Naoya,Kagoshima, Takanori,et al. Origin of methane-rich natural gas at the West Pacific convergent plate boundary[J]. SCIENTIFIC REPORTS,2017,7.
APA Sano, Yuji.,Kinoshita, Naoya.,Kagoshima, Takanori.,Takahata, Naoto.,Sakata, Susumu.,...&Pinti, Daniele L..(2017).Origin of methane-rich natural gas at the West Pacific convergent plate boundary.SCIENTIFIC REPORTS,7.
MLA Sano, Yuji,et al."Origin of methane-rich natural gas at the West Pacific convergent plate boundary".SCIENTIFIC REPORTS 7(2017).

入库方式: OAI收割

来源:地质与地球物理研究所

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