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Earth Processes
Published by the American Geophysical Union as part of the Geophysical Monograph Series, Volume 95. Publication of this monograph will coincide, to a precision of a few per mil, with the centenary of Henri Becquerel's discovery of "radiations actives" (C. R. Acad. Sci., Feb. 24, 1896). In 1896 the Earth was only 40 million years old according to Lord Kelvin. Eleven years later, Boltwood had pushed the Earth's age past 2000 million years, based on the first U/Pb chemical dating results. In exciting progression came discovery of isotopes by J. J. Thomson in 1912, invention of the mass spectrometer by Dempster (1918) and Aston (1919), the first measurement of the isotopic composition of Pb (Aston, 1927) and the final approach, using Pb-Pb isotopic dating, to the correct age of the Earth: close-2.9 Ga (Gerling, 1942), closer-3.0 Ga (Holmes, 1949) and closest-4.50 Ga (Patterson, Tilton and Inghram, 1953).
Mathematical Geodesy
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National Library of Medicine Current Catalog
First multi-year cumulation covers six years: 1965-70.
The Tectonic and Geologic Evolution of Southeast Asian Seas and Islands
Intended as a companion or sequel to the atlas " A Geophysical Atlas of East and South East Asia Seas" Provides the first interpretation of data contained in the atlas. It also presents many of the results obtained during the last several years of IDOE-supported feild experiments as well as imporatant and closely coordinated Deep Sea Drilling Project investigations developed during the international phase of Ocean Drilling.
Greenland Ice Core
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NOAA Week
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Federal Register
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Collected reprints
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