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CHEMICAL COMPOSITION OF DEEP FAULT FLUID AND EARTHQUAKE SOURCE FAULT

Research Project

Project/Area Number 11640413
Research Category

Grant-in-Aid for Scientific Research (C)

Allocation TypeSingle-year Grants
Section一般
Research Field 固体地球物理学
Research InstitutionShinshu University

Principal Investigator

TSUKAHARA Hiroaki  SHINSHU UNIVERSITY, DEPRTMENT OF ENVIRONMENTAL SCIENCES, PROFESSOR, 理学部, 教授 (20242711)

Co-Investigator(Kenkyū-buntansha) IKEDA Ryujl  NATIONAL RESEARCH INSTITUTE FOR EARTH SCIENCE AND DISASTER PREVENTION, RESEARCHER, 防災化学研究所, 研究職(室長)
SATAKE Hiroshi  TOYAMA UNIVERSITY,DEPARTMENT OF EARTH SCIENCE, PROFESSOR, 理学部, 教授 (40134994)
MORIKIYO Toshiro  SHINSHU UNIVERSITY, DEPARTMENT OF GEOLOGY, ASSOCIATE PROFESSOR, 理学部, 助教授 (90115379)
Project Period (FY) 1999 – 2000
Project Status Completed (Fiscal Year 2001)
Budget Amount *help
¥3,600,000 (Direct Cost: ¥3,600,000)
Fiscal Year 2000: ¥600,000 (Direct Cost: ¥600,000)
Fiscal Year 1999: ¥3,000,000 (Direct Cost: ¥3,000,000)
KeywordsEARTHQUAKE GROUNDWATER / EARTHQUAKE CHEMISTRY / MATSUSHIRO SWARM EARTHQUAKE / NAGANOKENSEIBU EARTHQUAKE / SPA GEOCHEMISTRY / FAULT GROUNDWATER CHEMISTRY / 断層地下水
Research Abstract

( 1 ) Upwelling waters in the Matsushiro earthquake swarm area are analized chemically and isotopically. The composition of the deep groundwater causing the earthqakes is estimated to be 310 meq/l for Na ion and 330 meq/l for Cl ion.
( 2 ) Chemical analysis for the hot springs in the Suwa Spa area along Itoigawa-Shizuoka Tectonic Line reveals that the ratios Na ion to Cl ion concentrations of all springs are almost the same. This indicates that the source of the individual many spring waters is the same deep hot groundwater.
( 3 ) Chemical composition of the water from the springs in the Naganokenseibu Earthquake area does not show the location of the earthquake fault. However, the concentration of SO_4 ion indicates the distance of the springs from the volcano, Ontake.
( 4 ) The ion concentrations of the hot water from Kurasitanoyu situated along Itoigawa-Shizuoka Tectonic Line are decreasing this year, 2000. Temperature is also decreasing. The reason has not revealed yet. The teasurments now continue.

Report

(3 results)
  • 2001 Final Research Report Summary
  • 2000 Annual Research Report
  • 1999 Annual Research Report
  • Research Products

    (5 results)

All Other

All Publications (5 results)

  • [Publications] 奥澤 保, 塚原弘昭: "松代群発地震地域に湧出する深層地下水"地震. 53. 241-253 (2001)

    • Description
      「研究成果報告書概要(和文)」より
    • Related Report
      2001 Final Research Report Summary
  • [Publications] 奥澤 保, 塚原弘昭: "松代群発地震地域に湧出する地下水の直下地震にともなう化学成分変化"温泉科学. 52(印刷中). (2002)

    • Description
      「研究成果報告書概要(和文)」より
    • Related Report
      2001 Final Research Report Summary
  • [Publications] OKUSAWA,TAMOTSU, TSUKAHARA,HlROAKI: "Origin of deep ground water in the Matsushiro earthquake swarm area ( in Jananese with English abstract )"Zisin ( J. Seismol. Soc. Japan ). 53. 241-253 (2001)

    • Description
      「研究成果報告書概要(欧文)」より
    • Related Report
      2001 Final Research Report Summary
  • [Publications] OKUSAWA,TAMOTSU, TSUKAHARA,HIROAKI: "Temporal variation in chemical composition of ground water from the Matsushiro Earthquake Swarm area at an earthquake ( in Japanese with English abstract )"J. Balneological Society of Japan. 52 (in press). (2002)

    • Description
      「研究成果報告書概要(欧文)」より
    • Related Report
      2001 Final Research Report Summary
  • [Publications] 奥澤保,塚原弘昭: "松代群発地震地域に湧出する深層地下水"地震. 53巻(印刷中). (2001)

    • Related Report
      2000 Annual Research Report

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Published: 1999-04-01   Modified: 2016-04-21  

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