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Dar al Gani meteorite | which depends on its composition | | | | | | | during meteor phase which depends on composition | Dar al Gani plateau, Libyan Sahara Desert | | | | can be severe due to long exposure time to environmental corrosion agents | | | DaG | | lower because the fall was not witnessed | 485755 kg | | in degrees, minutes and seconds of lattitude and longitude | | often minerals not found on Earth | Sahara meteorite | | when the meteorite was found | | | 1691 | meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal | directly proportional to initial velocity | | | | | |
eucrite | low | orthopyroxene, olivine, chromite; pigeonite, calcic plagioclase, silica | | | | | no chondrules | high because it is more friable than iron meteorite | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | | cumulates, crystallized melts, impact mixing | extrusion onto the surface of the planet or asteroid via a volcanic eruption | | | AUEC | | 7.1 % of meteorite falls | | 231 kg | | in degrees, minutes and seconds of lattitude and longitude | anorthite-pigeonite Ca-rich | silicates (with very few exceptions) | basalt | | | | | 23 | 4 Vesta | high because it is more friable than iron meteorite | | very rapid | | Howardite, Eucrite, Diogenite | coarse-grained orthopyroxenites, gabbros, fine- to coarse-grained basalts, brecciated |
S3 shock stage meteorite | which depends on its composition | | | weakly shocked | S3 | | | during meteor phase which depends on composition | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | shock metamorphism | | | | | | | | | 485755 kg | | in degrees, minutes and seconds of lattitude and longitude | | often minerals not found on Earth | shocked meteorite | | | | | 1691 | meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal | directly proportional to initial velocity | 15 to 20 GPa | | | | |
DaG 609 | which depends on its composition | orthopyroxene, olivine, chromite; pigeonite, calcic plagioclase, silica | 2 | weakly shocked | S3 | eucrite | no chondrules | during meteor phase which depends on composition | Dar al Gani plateau, Libyan Sahara Desert | shock metamorphism | cumulates, crystallized melts, impact mixing | extrusion onto the surface of the planet or asteroid via a volcanic eruption | can be severe due to long exposure time to environmental corrosion agents | W2 | AUEC | DaG | | lower because the fall was not witnessed | 231 kg | Fs% 27-63 | 26° 53.13' N. 16° 34.81' E. | anorthite-pigeonite Ca-rich | often minerals not found on Earth | | iron-rich, monomict, with chromite grains | 1998 | 0.696 kg |
 | 23 | 4 Vesta | directly proportional to initial velocity | 15 to 20 GPa | very rapid | A. Sexton, Open University, UK. A. Sexton, Meteoritical Bulletin No 83 | Howardite, Eucrite, Diogenite | coarse-grained orthopyroxenites, gabbros, fine- to coarse-grained basalts, brecciated |