Investigation on the correlated mechanisms between deep groundwater flow and material transport in the different plate tectonic fields
Project/Area Number |
20241006
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Research Category |
Grant-in-Aid for Scientific Research (A)
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Allocation Type | Single-year Grants |
Section | 一般 |
Research Field |
Environmental dynamic analysis
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Research Institution | Kyoto University |
Principal Investigator |
MAHARA Yasunori Kyoto University, 原子炉実験所, 教授 (30371537)
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Co-Investigator(Kenkyū-buntansha) |
TOKUNAGA Tomocjika 東京大学, 大学院・新領域創成学研究科, 准教授 (70237072)
MATSUZAKI Hiroyuki 東京大学, 大学院・工学研究科原子力専攻, 准教授 (60313194)
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Co-Investigator(Renkei-kenkyūsha) |
OHTA Tomoko 京都大学, 原子炉実験所, 助教 (30373020)
KUBOTA Takumi 京都大学, 原子炉実験所, 助教 (90335240)
NAKATA Eiji 財団法人電力中央研究所, 主任研究員 (80371409)
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Project Period (FY) |
2008 – 2010
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Project Status |
Completed (Fiscal Year 2010)
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Budget Amount *help |
¥36,920,000 (Direct Cost: ¥28,400,000、Indirect Cost: ¥8,520,000)
Fiscal Year 2010: ¥3,900,000 (Direct Cost: ¥3,000,000、Indirect Cost: ¥900,000)
Fiscal Year 2009: ¥9,750,000 (Direct Cost: ¥7,500,000、Indirect Cost: ¥2,250,000)
Fiscal Year 2008: ¥23,270,000 (Direct Cost: ¥17,900,000、Indirect Cost: ¥5,370,000)
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Keywords | 鹹水 / 沃素同位体比 / 塩素同位体比 / 希ガス / 付加体 / プレートテクトニクス / 希ガス濃度 / 地下水年代測定 / 海生有機物 / タービダイト / 溶存希ガス |
Research Abstract |
We collected brines from deep oil and natural gas reservoirs in forearc and backarc settings in the Japan arc and compared their ^<129>I/^<127>I, ^<36>Cl/Cl, dissolved noble gases and stable isotope (δD and δ^<18>O). We determined iodine ages of 22-53 Ma for brines from the backarc region by using an initial marine ^<129>I/^<127>I ratio of 1.5×10^<-12>. Because expansion of the Japan Sea started 25 Ma and ceased by 14 Ma, there is a great discrepancy between the iodine ages and the history of the formation of the Japan arc. We found no relationship between the ^<129>I/^<127>I ratio in deep brines and their tectonic settings.
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Report
(4 results)
Research Products
(30 results)
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[Journal Article] A multiple-isotope (δ^<37>Cl, ^<14>C, ^3H) approach to reveal the coastal hydrogeological system and its temporal changes in western Kyushu2011
Author(s)
Tokunaga, T., Shimada, J., Kimura, Y., Inoue, D., Mogi, K., Asai, K.
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Journal Title
Japan.Hydrogeol.J. 19
Pages: 249-258
Related Report
Peer Reviewed
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[Journal Article] Radionuclide in ancient relics obtained from the Matsuzaki site and the Hirohata shellmound on the Pacific coast of Japan.2010
Author(s)
Ohta T., Mahara Y., Kubota T., Saito Y., Fukutani S., Fujii T., Ando A., Nakata E., Nakano T., Abe Y., Tatematsu A.
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Journal Title
Radiocarbon 52
Pages: 526-533
Related Report
Peer Reviewed
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[Journal Article] Groundwater dating by estimation of groundwater flowvelocity and dissolved ^4He accumulation rate calibrated by ^<36>Cl in the Great Artesian Basin, Australia.2009
Author(s)
Mahara Y., Habermehl M. A., Hasegawa T., Nakata K., Ransley T. R., Hatano T., Mizuochi Y., Kobayashi H., Ninomiya A., Senior B. R., Yasuda H., Ohta T.
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Journal Title
Earth and Planetary Science Letters 287
Pages: 43-56
NAID
Related Report
Peer Reviewed
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[Journal Article] Physical Properties of the Shallow Sediments in the Late Pleistocene Formations, the Ursa Basin, Gulf of Mexico, and their Implications for Generation and Preservation of Shallow Overpressures.2009
Author(s)
Binh, N.T.T., Tokunaga, T., Nakamura, T., Kozumi, K., Nakajima, M., Kubota, M., Kameya, H., Taniue, M.
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Journal Title
Mar.Petrol.Geol. 26
Pages: 474-486
Related Report
Peer Reviewed
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[Presentation] Comparison among brines ages estimated from ^<36>Cl/Cl ratio, concentration of dissolved ^4He and 129I/127I ratio, and the origin of iodine in the Mobara Gasd field, Japan.2010
Author(s)
Mahara Y., Ohta T., Tokunaga T., Matsuzaki H., Nagao K., Nakata E.
Organizer
Proceedings of the 11th Workshop on Environmental Radioactivity(107-116)(in Japanese with English abstract)
Place of Presentation
KEK, Tsukuba, Japan.
Related Report
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