An attempt to establish a method for estimating the magma intrusion volume and the timing of eruption from volcano tectonic earthquakes
Project/Area Number |
18K03781
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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 17040:Solid earth sciences-related
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Research Institution | Kyoto University |
Principal Investigator |
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Project Period (FY) |
2018-04-01 – 2023-03-31
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Project Status |
Completed (Fiscal Year 2022)
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Budget Amount *help |
¥4,420,000 (Direct Cost: ¥3,400,000、Indirect Cost: ¥1,020,000)
Fiscal Year 2021: ¥780,000 (Direct Cost: ¥600,000、Indirect Cost: ¥180,000)
Fiscal Year 2020: ¥1,040,000 (Direct Cost: ¥800,000、Indirect Cost: ¥240,000)
Fiscal Year 2019: ¥1,170,000 (Direct Cost: ¥900,000、Indirect Cost: ¥270,000)
Fiscal Year 2018: ¥1,430,000 (Direct Cost: ¥1,100,000、Indirect Cost: ¥330,000)
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Keywords | 火山構造性地震 / 群発地震 / 地震エネルギー / 噴火時刻 / 地殻変動 / 体積変化量 / 応力場 / 噴出量 / ダイク / 破壊強度 / 機械学習 / 低周波地震 / 爆発地震 / 決定木 / 特徴量 / 非階層的クラスタリング法 / 桜島火山 / マグマ貫入 / 震源 / 発震機構 / 火山性地震 / マグマ貫入量 / 地震モーメント |
Outline of Final Research Achievements |
Volcano tectonic earthquakes originate from brittle fracture caused by stress changes in surrounding rocks due to magma intrusion. Magma intrusion causes not only a swam of volcano tectonic earthquakes and but also significant crustal deformation. An empirical equation is derived for the volume change of the deformation sources and seismic moment (energy) of volcano tectonic earthquakes. Using this empirical formula, we can estimate the volume of magma intrusion from observations of volcano tectonic earthquakes. The growth of a dike, a form of magma intrusion, increases the stress in the surrounding rocks, and the stress exceeds the fracture strength, which explains the occurrence process of volcano tectonic earthquakes. It is also revealed that a cluster of volcano tectonic earthquakes progressed from shallow to deep depths with the growth of the dike.
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Academic Significance and Societal Importance of the Research Achievements |
貫入したマグマの全てが噴火によって放出されるわけではないが,貫入マグマの量は放出しうるマグマ量の上限を規定する。噴火による放出量は災害の規模に関わるため,放出量の上限を事前に想定する意義がある。そのため,貫入マグマ量を推定することは重要であるが,地殻変動観測が不十分な発展途上国の火山であっても最低限は地震観測が行われているため,本研究成果の地震からのマグマ貫入量の推定手法の構築は意義がある。
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Report
(6 results)
Research Products
(18 results)
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[Journal Article] A Newly Installed Seismic and Geodetic Observational System at Five Indonesian Volcanoes as Part of the SATREPS Project2019
Author(s)
Nakamichi Haruhisa, Iguchi Masato, Triastuty Hetty, Kuswandarto Hery, Mulyana Iyan, Rosadi Umar, Gunawan Hendra, Suantika Gude, Aisyah Nurnaning, Budi-Santoso Agus, Nandaka I Gusti Made Agung
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Journal Title
Journal of Disaster Research
Volume: 14
Issue: 1
Pages: 6-17
DOI
NAID
ISSN
1881-2473, 1883-8030
Year and Date
2019-02-01
Related Report
Peer Reviewed / Open Access / Int'l Joint Research
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[Book] 住まいの百科事典2021
Author(s)
一般社団法人 日本家政学会 住居学部会
Total Pages
742
Publisher
丸善出版
ISBN
9784621305812
Related Report