IDPs' Silicate 10 µm Signature Versus Aliphatic 3.4 µm Features: A Key to Their Origin?

Details IDPs' Silicate 10 µm Signature Versus Aliphatic 3.4 µm Features: A Key to Their Origin? IDPs' Silicate 10 µm Signature Versus Aliphatic 3.4 µm Features: A Key to Their Origin?

Mar 2012

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2012lpi....43.1777m&link_type=abstract

43rd Lunar and Planetary Science Conference, held March 19–23, 2012 at The Woodlands, Texas. LPI Contribution No. 1659, id.1777

Computer Science

Scientific paper

Based on a quantification of olivine and pyroxene in the 10 µm
band of IDPs, we investigate a possible link between their mineral and
aliphatic components. This is probably reflecting an evolutionary
pathway of the studied particles.

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