Ikuo KushiroMJA[1] (久城 育夫, Kushiro Ikuo, born March 30, 1934, in Osaka Prefecture) is a Japanese petrologist, known for his research in experimental petrology. His experiments on peridotites contributed significantly to the understanding of the formation of magma under mid-ocean ridges and island arcs.[2][3]
Education and career
Between 1953 and 1957 Kushiro studied geology at the University of Tokyo. After graduation with a bachelor of science degree, he was a PhD student under Hisashi Kuno and studied the petrology of igneous rocks. After graduating with a doctorate in 1962, he worked for three years at the Carnegie Institution Geophysical Laboratory in Washington, D.C., specializing under the direction of J. Frank Schairer and Hatten Schuyler Yoder on experimental petrology. The central subject of his work was the formation of basaltic magmas with special consideration of the role of water. He and his colleagues identified phlogopite and potassium richterite (in which potassium is substituted for sodium in richterite) as two of the most important minerals involving in recycling water into the Earth's interior.[4] In 1967, after two years at the University of Tokyo, he returned to the Geophysical Laboratory as a postdoc and was employed there from 1971 to 1981 as a scientist. In 1969 he was involved in examining rock samples brought from the Moon by Apollo 11 as part of the Apollo program.[5] In 1974 he became a professor of petrology at the University of Tokyo while remaining an employee of the Carnegie Institution.
From 1990 to 1994, Kushiro was academic dean of the University of Tokyo, after which he was appointed vice president of the university. After retiring from the University of Tokyo, Kushiro became head of Okayama University's Institute for Study of the Earth's Interior (ISEI), where he remained until 1999. Since then he has worked as a director at the Institute for Frontier Research on Earth Evolution (IFREE) near Tokyo.
