【深発地震の発生メカニズム】プレート内の「見えない水の流れ」が深発地震とプレート大変形を制御していることを発見【岡山大学など】
Associate Professor Takayuki Ishii from the Graduate School of Natural Science and Technology at Okayama University, along with an international research team from Peking University and the Beijing High Pressure Science Research Center, recreated the environment inside the subducting plate through high-temperature and high-pressure experiments, revealing that the "movement of water" within the plate is significantly related to the occurrence of deep earthquakes.
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Associate Professor Takayuki Ishii from the Graduate School of Natural Science and Technology at Okayama University, along with an international research team from Peking University and the Beijing High Pressure Science Research Center, recreated the environment inside the subducting plate through high-temperature and high-pressure experiments, revealing that the "movement of water" within the plate is significantly related to the occurrence of deep earthquakes.