ALUMINUM-26 AS A PLANETOID HEAT SOURCE IN THE EARLY SOLAR SYSTEM
Author:
Publisher
Wiley
Subject
General Earth and Planetary Sciences,General Environmental Science
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1945-5100.1977.tb00464.x/fullpdf
Reference9 articles.
1. The record in the meteorites. III. On the development of meteorites in asteroidal bodies;Fish;Astrophys. J.,1960
2. Cooling rates and thermal histories of iron and stony-iron meteorites;Fricker;Geochim. Cosmochim. Acta,1970
3. Thermal models of inhomogeneously accreted meteorite parent bodies;Herndon;Nature Phys. Sci.,1973
4. Demonstration of 26Mg excess in Allende and evidence for 26Al;Lee;Geophys. Res. Lett.,1976
5. Aluminum-26 in the early solar system: fossil or fuel? Astrophys;Lee;J.,1977
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