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In page (450894) 2008 BT18:
"On 26 July 2008, observations at the IRTF using the SpeX-spectrograph showed that 2008 BT18 is a basaltic achondrite, suggesting that its parent body was subjected to sufficiently high temperatures to produce a eutectic melt.[1] The body's surface is thought to be dominated by iron-rich orthopyroxenes with little or no olivine.[1]
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