Thermal and material recycling process in the upper mantle beneath off-arc region
Project/Area Number |
23740398
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Research Category |
Grant-in-Aid for Young Scientists (B)
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Allocation Type | Multi-year Fund |
Research Field |
Petrology/Mineralogy/Science of ore deposit
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Research Institution | Osaka City University (2014-2015) Japan Agency for Marine-Earth Science and Technology (2011-2013) |
Principal Investigator |
Sakuyama Tetsuya 大阪市立大学, 大学院理学研究科, 准教授 (80553081)
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Project Period (FY) |
2011-04-28 – 2016-03-31
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Project Status |
Completed (Fiscal Year 2015)
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Budget Amount *help |
¥4,030,000 (Direct Cost: ¥3,100,000、Indirect Cost: ¥930,000)
Fiscal Year 2014: ¥650,000 (Direct Cost: ¥500,000、Indirect Cost: ¥150,000)
Fiscal Year 2013: ¥1,040,000 (Direct Cost: ¥800,000、Indirect Cost: ¥240,000)
Fiscal Year 2012: ¥1,040,000 (Direct Cost: ¥800,000、Indirect Cost: ¥240,000)
Fiscal Year 2011: ¥1,300,000 (Direct Cost: ¥1,000,000、Indirect Cost: ¥300,000)
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Keywords | アルカリ玄武岩 / プレート内火山 / スタグナントスラブ / ユーラシア大陸東縁部 / 海洋地殻 / 堆積物 / マントル遷移層 / 超背弧域 / 脱水した海洋地殻 / 流体 / 沈み込んだ堆積物 / 国際情報交換 / 北京大学 / 中国東北部地域 / アルカリ玄武岩火山 / 停滞スラブ / 上部マントル / 背弧火成活動 / 沈み込み堆積物 / 国際情報交流 / 中国東部地域 / HIMU玄武岩 |
Outline of Final Research Achievements |
Stagnation of the subducted Pacific slab in the mantle transition zone beneath eastern China has been imaged by seismic tomography. Late Cenozoic basaltic volcanoes lying above the stagnant slab, are distributed throughout eastern China. These basalts are rich in alkaline and incompatible trace elements that are typically associated with oceanic island basalts (OIBs). Such geochemical similarities between the basalts in eastern Asia and typical OIBs have led some researchers to conclude that the Chinese basalts originated from the upwelling of mantle, independent of a stagnant slab. According to the results of high-pressure experiments, melting of the stagnant slab could occur if the slab contains adequate amounts of H2O or CO2. In this study, we presented geochemical and petrological evidence that melts from the igneous layers in the stagnant Pacific plate slab have contributed to the source composition of basalts erupted in eastern China.
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Report
(6 results)
Research Products
(16 results)
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[Journal Article] Melting of the Uppermost Metasomatized AsthenosphereTriggered by Fluid Fluxing from Ancient Subducted Sediment: Constraints from the Quaternary Basalt Lavas at Chugaryeong Volcano, Korea2014
Author(s)
Tetsuya Sakuyama, Shinji Nagaoka, Takashi Miyazaki, Qing Chang, Toshiro Takahashi, Yuka Hirahara, Ryoko Senda, Tetsumaru Itaya, Jun-Ichi Kimura, Kazuhito Ozawa
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Journal Title
Journal of Petrology
Volume: 55
Issue: 3
Pages: 499-528
DOI
Related Report
Peer Reviewed
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[Journal Article] Melting of dehydrated oceanic crust from the stagnant slab and2013
Author(s)
Tetsuya Sakuyama, Wei Tian, Jun-Ichi Kimura, Yoshio Fukao, Yuka Hirahara, Toshiro Takahashi, Ryoko Senda, Qing Chang, Takashi Miyazaki, Masayuki Obayashi, Hiroshi Kawabata, Yoshiyuki Tatsumi
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Journal Title
Chemical Geology
Volume: 359
Pages: 32-48
DOI
Related Report
Peer Reviewed
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[Presentation] Melting of the oceanic crust in the stagnant slab at the mantle transition zone: Constraints from alkaline basalts in eastern China2011
Author(s)
Tetsuya Sakuyama, Wei Tian, Jun-Ichi Kimura, Yoshio Fukao, Yuka Hirahara, Toshiro Takahashi, Ryoko Senda, Qing Chang, Takashi Miyazaki, Masayuki Obayashi, and Yoshiyuki Tatsumi
Organizer
AGU fall meeting 2011
Place of Presentation
Moscone Center, San Francisco
Related Report
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[Presentation] Melting of a stagnant slab in the mantle transition zone: Constraints from Cenozoic alkaline basalts in eastern China
Author(s)
Tetsuya Sakuyama, Wei Tian, Jun-Ichi Kimura, Yoshio Fukao, Yuka Hirahara, Toshiro Takahashi, Ryoko Senda, Qing Chang, Takashi Miyazaki, Masayuki Obayashi, Hiroshi Kawabata, Yoshiyuki Tatsumi
Organizer
IAVCEI2013 Scientific Assembly
Place of Presentation
かごしま県民交流センター(鹿児島県)
Related Report
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