Paleomagnetic geochronology and its applications to tsunami boulders and fault gouges
Project/Area Number |
18K03755
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Research Category |
Grant-in-Aid for Scientific Research (C)
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Allocation Type | Multi-year Fund |
Section | 一般 |
Review Section |
Basic Section 17030:Human geosciences-related
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Research Institution | Tohoku University |
Principal Investigator |
Nakamura Norihiro 東北大学, 高度教養教育・学生支援機構, 教授 (80302248)
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Co-Investigator(Kenkyū-buntansha) |
後藤 和久 東京大学, 大学院理学系研究科(理学部), 教授 (10376543)
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Project Period (FY) |
2018-04-01 – 2021-03-31
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Project Status |
Completed (Fiscal Year 2020)
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Budget Amount *help |
¥4,290,000 (Direct Cost: ¥3,300,000、Indirect Cost: ¥990,000)
Fiscal Year 2020: ¥650,000 (Direct Cost: ¥500,000、Indirect Cost: ¥150,000)
Fiscal Year 2019: ¥1,040,000 (Direct Cost: ¥800,000、Indirect Cost: ¥240,000)
Fiscal Year 2018: ¥2,600,000 (Direct Cost: ¥2,000,000、Indirect Cost: ¥600,000)
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Keywords | 古地磁気学 / 津波性巨礫 / ナノバブル / 巨礫 / 津波 / 泥流堆積物 / 年代決定 / 粘性残留磁気 / ラハール / 地磁気年代 / 古地磁気年代 |
Outline of Final Research Achievements |
We have developed a paleomagnetic viscous dating with a stretched exponential relaxation for various grain-size distributions of magnetite. Also we have developed the effective method of reductive chemical demagnetization with a nano-bubble generator. These two methods allowed us to determine the date of tsunamigenic boulder. Examination of the tsunamigenic coral boulders, whose emplacement ages are determined by radiocarbon, has revealed the age estimated from paleomagnetic viscous dating indicates an older age. The stretched exponential relaxation method we have developed succeeded to explain the older ages. Our newly-developed nano-bubble method for reductive chemical demagnetization of volcanic rocks revealed two components, the characteristic remanence during the eruption and the viscous remanence acquired after the emplacement. We found that many boulders are distributed along the coral reefs of the western coast of Eua island where is located western side of the Tonga trench.
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Academic Significance and Societal Importance of the Research Achievements |
三陸沿岸には多くの巨礫があり,その巨礫を祀る神社が多い。これは巨大津波を経験した先人が,未来の私たちに宗教儀式として,津波の危険性を知らせるためのタイムマシーンなのだろう。しかし,津波の危険性は理解できても,「いつ・どれぐらいの規模」の津波が襲ったのかの定量的なデータはわからない。さらに,巨礫が移動したことから規模は推定できても,「いつ」については推定する術がこれまでなかった。本研究にいたるこれまでの地磁気による年代推定研究により,巨礫ひとつから「いつ・どれぐらいの規模」の津波が発生したことを推定できる手法を開発した。これにより,宗教的なお祀りだけでなく,津波に関する定量的な知識が得られる。
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Report
(4 results)
Research Products
(15 results)
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[Presentation] Dating of tsunami boulders from Ishigaki Island, Japan, with a stretched exponential relaxation approach2018
Author(s)
Sato T., Nakamura N., Kumagai Y., Goto K., Nagahama H., Minoura K., Zhao X., Heslop D., and Roberts A. P.
Organizer
American Geophysical Union
Related Report
Int'l Joint Research
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