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Geophysical Laboratory Carnegie Institution of Washington

Geophysical Laboratory, Carnegie Institution of Washington, 5251 Broad Branch RoadNW, Washington, DC 20015, USA... [Pg.409]

Institute for Advanced Research, Nagoya University, Nagoya 464-8601, Japan " Institute for Solid State Physics, University of Tokyo, Kashiwa, Chiba 277-8581, Japan. Geophysical Laboratory, Carnegie Institution of Washington, Washington, DC 20015, USA... [Pg.469]

T. N. Irvine, ed.. Chromium Its Physicochemical Behavior and Petrologic Significance, Carnegie Institution of Washington Conference, Geophysical Laboratory, Pergamon Press, Inc., Elmsford, N.Y., 1977. [Pg.130]

Hare, PE. and von Endt, D. 1990 Variable preservation of organic matter in fossil bone. Annual Report of the Director of the Geophysics Laboratory. Carnegie Institution, Washington. 1989-1990. Washington, D.C., Carnegie Institution ofWashington 115-118. [Pg.86]

Fogel, M L., Tuross, N. and Owsley, D.W. 1989 Nitrogen isotope tracers of human lactation in modern and archaeological populations. Annual Report of the Director, Geophysical Laboratory, Carnegie Institution, Washington D.C. 1988-1989 111-117. [Pg.257]

Arthur L. Day to John C. Merriam, 26 July 1930, Geophysical Laboratory Projects—High Pressure Research Program, files of the Carnegie Institution of Washington, Washington, D. C. [Pg.33]

Fig. 2.10B. From Morimoto, N. (1959). The structural relations among 3 polymorphs of MgSiOs—enstatite, protoenstatite and clinoenstatite. Fig. 62, p. 198. In Report of the Director, Geophysical Laboratory, 1958-59. Carnegie Institution Year Book 58, Washington, D.C. With permission of Carnegie Institution of Washington. Fig. 2.10B. From Morimoto, N. (1959). The structural relations among 3 polymorphs of MgSiOs—enstatite, protoenstatite and clinoenstatite. Fig. 62, p. 198. In Report of the Director, Geophysical Laboratory, 1958-59. Carnegie Institution Year Book 58, Washington, D.C. With permission of Carnegie Institution of Washington.
I- 19 and J.W. Servos, To explore the borderland The foundation of the Geophysical Laboratory of the Carnegie Institution of Washington, Historical Studies in the Physical Sciences 14 (1983) 147-185. [Pg.184]

THE AVERAGE CHEMICAL COMPOSITION OF IGNEOUS ROCKS. By Frank W. Clarke and Henry S. Washington U. S. Geological Survey and Geophysical Laboratory of the Carnegie Institution of Washington Communicated March 22, 1922... [Pg.1]

It is of interest to Earth scientists that one of the most prestigious laboratories in the field of experimental petrology and geochemistry, the Geophysical Laboratory of the Carnegie Institution of Washington, has its own practical temperature scale. This was developed in 1914 by Arthur L. Day, based on earlier measurements with a gas thermometer by Day and Sosman, and these same fixed points have been used at the... [Pg.66]

Quite recently, researchers from the Max Plank Institute for Chemistry and the Geophysical Laboratory at the Carnegie Institution of Washington reported the polymerization of nitrogen in sodium azide [16-18]. With increasing pressure on sodium azide, the sample became completely opaque above... [Pg.88]

Bell, P., and G. Nord (1974). Microscopic and Electron Diffraction Study of Fi-brolitic Sillimanite, pp. 443-446. Report of the Director, 1973-1974. Geophysical Laboratory, Yearbook No. 73, Carnegie Institute, Washington, DC. Bernal, J. D. (1924). The structure of graphite. Proc. Roy. Soc. London A 106 749-... [Pg.96]


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