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Ikuo Kushiro

Ikuo Kushiro is a astronomy topic covered in the lgStudy science library. This page brings together a partial reference excerpt, illustrations, worked examples, real-world applications and a short study plan, so you can understand Ikuo Kushiro rather than just read about it. In short: Ikuo Kushiro MJA (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.

Ikuo Kushiro — main illustration
Ikuo Kushiro — illustration

Key takeaways

  • Ikuo Kushiro belongs to astronomy; place it in that map before memorising details.
  • Learn the definition first, then one example that makes the definition concrete.
  • Connect Ikuo Kushiro to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Ikuo Kushiro from memory before moving on to harder problems.

Reference excerpt

Ikuo Kushiro MJA (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.

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. 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. 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.

Awards and honors Kushiro was elected in 1976 a Fellow of the American Geophysical Union. In 1982, he received the Japan Academy Prize. He was elected in 1983 to the National Academy of Sciences and in 1993 to the Japan Academy. In 1997 he became an honorary member of the Geochemical Society and the European Association of Geochemistry. In 1999 he received the Harry H. Hess Medal from the American Geophysical Union, and in the same year the Roebling Medal of the Mineralogical Society of America and the Arthur Holmes Medal of the European Union of Geosciences. He won the V. M. Goldschmidt Award in 2001. In 2003 the Geological Society of London awarded him the Wollaston Medal. In 2009 he was awarded the Japanese Order of the Sacred Treasure, 2nd Class. The same year, from a meteorite collected in Antarctica, a newly discovered mineral from the pyroxene group was named kushiroite in his honor.

Selected publications I. Kushiro (1960) Si-Al relation in clinopyroxenes from igneous rocks Am. J. Sci. 258, 548–54. I. Kushiro and H.S. Yoder (1966) Anorthite-forsterite and anorthite-enstatite reactions and their bearing on the basalt-eclogite transformation. J. Petrol. 7, 337–62. I. Kushiro (1968) Compositions of magmas formed by partial zone melting in the Earth's upper mantle. J. Geophys. Res. 73, 619–34. I. Kushiro, Y. Syono and S. Akimoto (1968) Melting of a peridotite nodule at high pressures and high water pressures. J. Geophys. Res. 73, 6023–29. I. Kushiro (1969) The system forsterite-diopside-silica with and without water at high pressures. Am. J. Sci. 267A, 269–94. I. Kushiro and H. Haramura (1971) Major element variation and possible source materials of Apollo 12 crystalline rocks. Science 171, 1235–1237. I. Kushiro (1972) Effect of water on the composition of magmas at high pressures. J. Petrol. 13, 311–34. I. Kushiro (1975) On the nature of silicate melt and its significance in magma genesis. Am. J. Sci. 275, 411–31. I. Kushiro (1976) Change in viscosity and structure of melt of NaAlSi2O6 composition at high pressures. J. Geophys. Res. 81, 6347–50. I. Kushiro (1990) Partial melting of mantle wedge and evolution of island arc crust. J. Geophys. Res. 95, 15929–39. I. Kushiro (1996) Partial melting of a fertile mantle peridotite at high pressures. Monogr. Am. Geophys. Union 95, 109–22. I. Kushiro (2001) Partial melting experiments on peridotite and origin of mid-ocean ridge basalt. Ann. Rev. Earth. Planet. Sci. 29, 71–107.

References

Illustrations

Ikuo Kushiro: Ikuo Kushiro
Ikuo Kushiro

Worked examples

Example 1 — a first encounter with Ikuo Kushiro

Start with the simplest possible case. Write down what Ikuo Kushiro claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In astronomy, the smallest case is usually a single object, a single equation or a single measurement. Check that every symbol or term in your sentence has a meaning in that case.

Example 2 — changing one variable

Take the situation from Example 1 and change exactly one quantity: double it, halve it, or set it to zero. Predict what should happen to Ikuo Kushiro before you calculate. Comparing your prediction with the result is the fastest way to find out whether you understand the idea or only the words.

Example 3 — an exam-style question

Typical questions about Ikuo Kushiro ask you to (a) state it precisely, (b) apply it to given data, and (c) explain a limitation. Practise writing all three answers in under five minutes; the third part is what separates a full-mark answer from an average one.

Applications of Ikuo Kushiro

In research
Ikuo Kushiro appears in astronomy research whenever the underlying quantities have to be modelled precisely. Papers usually cite it as a starting assumption and then explore where it breaks down.
In technology and industry
Engineering practice reuses Ikuo Kushiro in design rules, simulations and safety margins. Knowing the idea lets you read a specification sheet and understand why the numbers look the way they do.
In the classroom
Ikuo Kushiro is common in secondary-school and first-year university syllabi. It links to neighbouring topics 1934 births, Academic staff of the University of Tokyo, Fellows of the American Geophysical Union, so understanding it makes those chapters shorter.
In everyday life
Look for Ikuo Kushiro outside the textbook — in sport, cooking, traffic, electronics or the sky above you. An example you found yourself is remembered far longer than one you were given.

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How to study Ikuo Kushiro in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Ikuo Kushiro means in your own words.
  3. Compare your version with the excerpt and mark what you missed.
  4. Work through the three examples above with pen and paper.
  5. Explain Ikuo Kushiro out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Ikuo Kushiro in simple terms?

Ikuo Kushiro MJA (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 arc…

Why does Ikuo Kushiro matter?

Because it connects several astronomy ideas at once: it gives you a definition you can apply, a quantity you can calculate, and a way to check whether a result is plausible.

How should I study Ikuo Kushiro?

Read the excerpt, restate it from memory, then work through the examples and applications listed on this page. The five-step study plan above takes about twenty minutes.

What does this page cover?

It gives you a compact reference excerpt plus original lgStudy explanations, examples, applications and study material on Ikuo Kushiro.

Tags

  • 1934 births
  • Academic staff of the University of Tokyo
  • Fellows of the American Geophysical Union
  • International members of the National Academy of Sciences
  • Japanese geologists
  • Living people
  • Members of the Japan Academy
  • Petrologists
  • Recipients of the Order of the Sacred Treasure, 2nd class
  • Recipients of the V. M. Goldschmidt Award
  • Scientists from Osaka Prefecture
  • University of Tokyo alumni

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