北部フォッサマグナ地域における深層地下水の水質特性

書誌事項

タイトル別名
  • Geochemical Characteristics of Deep Groundwater in the Northern Fossa Magna Region
  • ホクブ フォッサマグナ チイキ ニ オケル シンソウ チカスイ ノ スイシツ トクセイ

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抄録

The deep ground water in the northern Fossa Magna region where thick formations in the Neogene and later periods are distributed is represented by Na·Cl type groundwater originating from fossil seawater.<BR>The high-density Na-Cl type groundwater has risen to a shallow depth under the ground surface. Monitoring the electric conductivity of the groundwater could help identify the geological structures such as active faults.<BR>The Cl concentration in strong salt springs that are mixed with little meteoric water decreases, and δ18O increases in formations of later geological periods. Measuring the Cl concentration and δ18O could therefore enable the estimation of the period of the fossil seawater from which the strong salt spring originates, and may be effective for determining the rock from which hot spring seepage occurs.

収録刊行物

  • 応用地質

    応用地質 45 (1), 22-30, 2004

    一般社団法人 日本応用地質学会

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