Part 4
Part 4
Part 4
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Meteorites<br />
! Largely, meteorites are residue from Solar System formation and condensation<br />
! Comprise a wide range of compositions, which formed at various epochs in our<br />
system’s s early history<br />
! Chondrites<br />
• Most common type of meteorite, date to 4.5 Ga<br />
• Undifferentiated, congealed directly by condensation from solar nebula<br />
• Relative concentrations of elements is close to solar (sans H, He)<br />
! Achondrites<br />
! Irons<br />
• <strong>Part</strong>ially differentiated meteorites<br />
• May derive from planetoids that underwent partial chemical differentiation<br />
• Differ in mineral composition<br />
• Thought to derive from earliest phases of solar nebula condensation, or from cores of<br />
differentiated planetoids that were subsequently shattered by impact<br />
! Carbonaceous Chondrites<br />
• Most primitive meteorites, fairly rare<br />
• Contain abundant organic carbon, amino acids, hydrocarbons… retained from condensation<br />
in early solar system evolution in outer system