Not exact matches
Of the 731 rock samples the Apollo 16 astronauts brought home in April 1972, nearly all were breccia, composites formed of
fragments fused together — probably
by the heat and pressure of
meteorite impacts.
Pizzarello and her team hydrothermally treated
fragments of the
meteorite and then detected the compounds released
by gas chromatography - mass spectrometry.
After the meteor was sighted streaking through the sky on 22 April,
meteorite hunters found
fragments of the rock, identified
by the «fusion crust» that forms when it burns in the atmosphere.
The graphite
fragments, Steele says, «are a remnant of basically a carbon - rich dust after an impact from a
meteorite containing carbon, or the carbon may have condensed from a gas» released
by an impact.
At that size, 2008 TC3 was always likely to be destroyed in the atmosphere — although some
fragments may have survived to fall as
meteorites — but the collision may help to highlight the risks posed
by larger bodies.