An achondrite is a stony meteorite that does not contain chondrules. It consists of material similar to terrestrial basalts or plutonic rocks and has been differentiated and reprocessed to a lesser or greater degree due to melting and recrystallization on or within meteorite parent bodies. As a result, achondrites have distinct textures and mineralogies indicative of igneous processes.

Achondrites account for about 8% of meteorites overall, and the majority (about <math>2/3</math>) of them belong to the HED clan, possibly originating from the crust of asteroid Vesta. Other types include Martian, Lunar, and several types thought to originate from as-yet unidentified asteroids. These groups have been determined on the basis of e.g. the Fe/Mn chemical ratio and the <sup>17</sup>O/<sup>18</sup>O oxygen isotope ratios, thought to be characteristic "fingerprints" for each parent body.

Classification

Achondrites are classified into the following groups:

  • Primitive achondrites
  • Asteroidal achondrites
  • Lunar meteorites
  • Martian meteorites

Primitive achondrites

Primitive achondrites, also called PAC group, are so-called because their chemical composition is primitive in the sense that it is similar to the composition of chondrites, but their texture is igneous, indicative of melting processes. To this group belong: They are named after the initial letters of the three subgroups:

  • Howardites
  • Eucrites
  • Diogenites
  • Angrites
  • Aubrites

Lunar meteorites

Lunar meteorites are meteorites that originated from the Moon.

Martian meteorite

Martian meteorites are meteorites that originated from Mars. They are divided into three main groups, with two exceptions (see last two entries):

  • Shergottites
  • Nakhlites
  • Chassignites
  • OPX martian meteorites (ALH 84001)
  • Regolith/Soil samples (NWA 7034 and pairings)

See also

  • Glossary of meteoritics

References

  • Achondrite Images from Meteorites Australia