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Murray Gell-Mann

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United States physicist noted for his studies of subatomic particles (born in 1929)

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Murray Gell-Mann

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In 1963, Wu investigated and confirmed the Conserved Vector Current hypothesis of Richard Feynman and Murray Gell-Mann.
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The quark model was independently proposed by physicists Murray Gell-Mann and George Zweig in 1964.
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Murray Gell-Mann proposed the formula independently in 1956.
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The term complex adaptive system was coined at the interdisciplinary Santa Fe Institute (SFI), by John H. Holland, Murray Gell-Mann and others.
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Murray Gell-Mann always referred to Feynman diagrams as Stueckelberg diagrams, after a Swiss physicist, Ernst Stueckelberg, who devised a similar notation many years earlier.
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The larger symmetry was named the Eightfold Way by Murray Gell-Mann, and was promptly recognized to correspond to the adjoint representation of SU(3).
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Cabibbo addressed these issues, following Murray Gell-Mann and Maurice Lévy, by postulating weak universality, which involves a similarity in the weak interaction coupling strength between different generations of particles.
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In 1957, Robert Marshak and George Sudarshan and, somewhat later, Richard Feynman and Murray Gell-Mann proposed a V−A (vector minus axial vector or left-handed) Lagrangian for weak interactions.
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When the quark model was first postulated by Murray Gell-Mann and others in the 1960s, it was to organize the states known then to be in existence in a meaningful way.
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The sentence "Three quarks for Muster Mark!" in Joyce's Finnegans Wake is the source of the word "quark", the name of one of the elementary particles proposed by the physicist Murray Gell-Mann in 1963.
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The name pentaquark was coined by Claude Gignoux et al. and Harry J. Lipkin in 1987; however, the possibility of five-quark particles was identified as early as 1964 when Murray Gell-Mann first postulated the existence of quarks.
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Murray Gell-Mann: Well, I would guess that modern language must be older than the cave paintings and cave engravings and cave sculptures and dance steps in the soft clay in the caves in Western Europe, in the Aurignacian Period some 35,000 years ago, or earlier.
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