Episode Description from the Publisher
「地下に注いだ水はじわじわ深くしみ込み、地震もだんだん深くなる」。これまで多くの研究者がそう考えてきました。ところが最新の研究で、その常識が平均値の生んだ見かけの姿にすぎなかったことが明らかになり、科学の面白さと落とし穴が同時に見えてきます。Nature CommunicationsPermeability heterogeneity controls fluid migration and microseismicity evolution in The Geysers geothermal field, California
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