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Grains of Meteorites, Originating in Cool Carbon Stars

Published online by Cambridge University Press:  12 April 2016

Uffe G. Jørgensen*
Affiliation:
Niels Bohr Institute, Blegdamsvej 17, DK-2100 Copenhagen, Denmark

Extract

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The bulk of meteorites consist of material that condensed out of the primitive solar nebula, and their isotopic composition is therefore similar to that of the sun. Unfractionated meteorites (carbonaceous chondrites), nevertheless, contain a small fraction of inclusions that have a distinctly different isotopie composition of carbon, xenon, krypton and other elements (Zinner et al., 1987). These inclusions are therefore believed to be of pre-solar origin, and their composition and mineralogical structure carries information about the place where they were born.

Type
5. Chromospheres, Winds and Mass Loss
Copyright
Copyright © Cambridge University Press 1989

References

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