Subject |
is paired with |
has shock texture |
has reference |
has degree of shock metamorphism |
has shock stage |
is an instance of |
has fall location |
has metamorphism mechanism |
has name |
has shock diagnostic mineral |
has olivine composition |
has olivine shock metamorphism |
has weathering stage |
has acronym |
has total mass of find |
has fall coordinate |
has find date |
has mass |
has image |
has augite composition |
has number of find |
has shock pressure |
has pigeonite composition |
has pyroxene content |
DaG 319 | | silicates show minor fracturing, undulatory extinction and kink bands primarily in olivine | | unshocked | S1 | S1 shock stage meteorite | Dar al Gani plateau, Libyan Sahara Desert | shock metamorphism | DaG 319 | small euhedral graphite crystals can sometimes be distinguished | | fracturing, undulatory extinction and kink bands | W2 | DaG | 9 kg (out of date) | 27° 01.68' N., 16° 21.52' E. | 1997 | 0.740 kg |
 | | 6 (out of date) | less than 5 GPa | | |
EET 83309 | | | Prinz et al. (1987) | | | Antarctic meteorite | Elephant Moraine, Antarctica | | EET 83309 | | Fo% 80-84 for monomict ureilitic clasts | | | | 485755 kg | in degrees, minutes and seconds of lattitude and longitude | 1983 | | | | 1691 | | Wo% variable En% variable for monomict ureilitic clasts | 0.27 in modal pyroxene/(pryroxene+olivine) for monomict ureilitic clasts |
EET 87720 | | | Warren and Kallemeyn (1991), AMN 12-3, AMN 13-1 | | | Antarctic meteorite | Elephant Moraine, Antarctica | | EET 87720 | | Fo% 79-87 | | | | 485755 kg | in degrees, minutes and seconds of lattitude and longitude | 1987 | | | Wo% 35 En% 52 | 1691 | | Wo% 8.0 En% 83 | |
Nilpena | North Haig meteorite (possibly) | | Jaques and Fitzgerald (1982) | | | polymict ureilite | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | | Nilpena | | Fo% 80 for monomict ureilitic clasts | | | | 485755 kg | in degrees, minutes and seconds of lattitude and longitude | when the meteorite was found | | | | 1691 | | Wo% 9.0 En% 75 for monomict ureilitic clasts | |
North Haig | Nilpena meteorite (possibly) | | Berkley et. al (1980) | | | polymict ureilite | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | | North Haig | | Fo% 76-92 | | | | 485755 kg | in degrees, minutes and seconds of lattitude and longitude | when the meteorite was found | | | | 1691 | | Wo% variable En% variable | 0.26 in modal pyroxene/(pryroxene+olivine) |