Hostname: page-component-848d4c4894-cjp7w Total loading time: 0 Render date: 2024-06-19T15:48:22.525Z Has data issue: false hasContentIssue false

4. A Chemical and Textural Comparison between Carbonaceous Chondrites and Interplanetary Dust

Published online by Cambridge University Press:  12 April 2016

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

Interplanetary dust probably has a cometary origin. Collectible samples of this material are likely to be more representative of the meteoroid complex than are meteorites. Since 1974, NASA U-2 spacecraft has been able to collect over 200 interplanetary particles in the stratosphere. Roughly 10% have spheroidal shapes indicating previous melting. The rest seems to come from the gentle fragmentation of a single type of parent-body material: a black aggregate of grains mainly 1000 A in size, whose properties are closely similar to C1 and C2 chondritic material.

Type
Part III. Meteors and Meteoroids
Copyright
Copyright © A.H. Delsemme 1977

References

Anders, E. 1975, Icarus. 24, 363.Google Scholar
Armstrong, J. T., and Buseck, P. R. 1975, Theoretical Anal. Chemistry, 47, 2178.Google Scholar
Brownlee, D. F., Horz, F., Tomandl, D., and Hodge, P. W. 1976, p. 962, NASA SP-393.Google Scholar
Brownlee, D. E., Tomandl, D., Hodge, P. W. 1976, p. 279, in IAU Colloquium 31, Interplanetary Dust and Zodiacal Light, ed. Elsasser and Fechtig, publ. Springer Verlag.Google Scholar
Chapman, C. R. 1976, Geochim. Cosmochim. Acta, 40, 701.Google Scholar
Fuchs, L. H., Olsen, E., and Jensen, K. J. 1973, Smithsonian Center for the Earth Sciences, 10.Google Scholar
Millman, P. M. 1972, p. 157 in Nobel Symposium 21: From Plasma to Planet, edit. A. Elvius, publ. Wiley & Sons.Google Scholar
Rajan, R. S., Brownlee, D. E., Tomandl, D., Hodge, P. W., Farrar, H., and Britten, R. A. 1977, Nature, in press.Google Scholar
Wetherill, G. W. 1974, Ann. Rev. Earth Planet. Sci., 2, 303.Google Scholar
Whipple, F. L. 1951, The Theory of Micrometeorites, Proc. Nat. Acad. Sci., USA, 37.Google Scholar
Whipple, F. L. 1967, p. 409, in Zodiacal Light and Interplanetary Medium, edit. J. L. Weinberg, publ. NASA SP-150.Google Scholar