Uranium concentration and distribution in six peridotite inclusions of probable mantle origin
Author:
Publisher
Elsevier BV
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics
Reference37 articles.
1. Lead concentration and isotopic composition in five peridotite inclusions of probable mantle origin;Zartman;Earth Planet. Sci. Letters,1973
2. Dependence of the surface heat flow on the radioactivity of the Earth;MacDonald;J. Geophys. Res.,1964
3. Relative contributions of uranium, thorium, and potassium to heat production in the Earth;Wasserburg;Science,1964
4. Speculations on the Earth's thermal history;Birch;Geol. Soc. Am. Bull.,1965
5. The implications of terrestrial heat flow observations on current tectonic and geophysical models of the crust and upper mantle of the Earth;Sclater;Geophys. J.,1970
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1. Extreme 176Hf/177Hf in the sub-oceanic mantle;Earth and Planetary Science Letters;1995-01
2. Mantle phlogopite: a significant lead repository?;Chemical Geology;1993-06
3. Implanted 3He, 4He, and Xe in further studies of diamonds from Western Australia;Geochimica et Cosmochimica Acta;1991-07
4. U-Th-Pb partitioning behavior during partial melting in the upper mantle: Implications for the origin of high Mu Components and the “Pb Paradox”;Journal of Geophysical Research;1990
5. Chemical and Isotopic Studies of Ultramafic Inclusions from the San Carlos Volcanic Field, Arizona: A Bearing on their Petrogenesis;Journal of Petrology;1989-08-01
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