High abundances of presolar silicates in Antarctic micrometeorites; implications for their cometary origins

Yada T., Stadermann F. J., Floss C., Zinner E., Nakamura T., Noguchi T., and Lea A. S. (2006) Lunar Planet. Sci. XXXVII, Abstract #1470.


ABSTRACT

Micrometeorites are the dominant type of extraterrestrial material accreting onto the Earth. Their parent bodies are thought to be asteroids and comets, although the mineralogical and chemical studies indicate that most should have originated from asteroids because of their similarities to carbonaceous (C) chondrites. We previously reported the presence of presolar silicates in Antarctic micrometeorites (AMMs). Here, we present a revised abundance of presolar silicates in AMMs and compare it with that of both anhydrous interplanetary dust particles (IDPs), which are thought to be of cometary origin, and C chondrites, in order to constrain the parent bodies of AMMs.


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