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个人简介
In the midst of the 20th-century Earth science-revolution of seafloor spreading theory and plate tectonics, he conducted diverse research in various fields of solid Earth science, including geo-electromagnetics, geothermics, and tectonics, and greatly contributed to the creation of a "new view of the Earth". Even after the establishment of plate tectonics, he continued to pursue a newer view of the Earth, promoting research based on novel ideas one after another and leading the Earth science community in the world.
His early research was mainly on rock magnetism. One of the most important of these studies was the discovery of thermoremanent magnetization (TRM) directed opposite to the magnetic field and that this phenomenon, self-reversal TRM, is a peculiar property of certain magnetic minerals. This result became his dissertation, and he was awarded the Tanakadate Prize of the Society of Terrestrial Magnetism and Electricity of Japan (1953).
His early research was mainly on rock magnetism. One of the most important of these studies was the discovery of thermoremanent magnetization (TRM) directed opposite to the magnetic field and that this phenomenon, self-reversal TRM, is a peculiar property of certain magnetic minerals. This result became his dissertation, and he was awarded the Tanakadate Prize of the Society of Terrestrial Magnetism and Electricity of Japan (1953).
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