黄檗断層付近のγ線測定

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書誌事項

タイトル別名
  • γ-RAY SURVEY AROUND THE OHBAKU FAULT
  • オウバク ダンソウ フキン ノ ガンマセン ソクテイ

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A γ-ray survey was carried out using a handy type scintillation survey meter around theOhbaku fault, where the under ground structure had been made clear by seismic explorationand gravity survey.Six traversal lines were chosen to cross the fault. Most distinguishable peak of the γ-rayintensity appeared on the observation point M 59, midst of the main line. This peak seemsto be caused by the high content of radon in the fault zone.Maximum peak in each of the six traverses located almost in a straight line, from NW toSE, and this must be the strike of the Ohbaku fault.

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