Subject |
is paired with |
has olivine inclusion |
has sediment mechanism |
has reference |
has degree of shock metamorphism |
has shock stage |
is an instance of |
has orthopyroxene composition |
has fall location |
has name |
has olivine composition |
has weather |
has weathering stage |
has acronym |
has texture |
has value |
has total mass of find |
has pronunciation |
has matrix composition |
has fall coordinate |
is a kind of |
has find date |
has mass |
has image |
has augite composition |
has origin |
has number of find |
has shock pressure |
has lithic clast composition |
has plagioclase |
has pigeonite composition |
has intergranular boundary |
has gain size |
has pyroxene content |
has pyroxene inclusion |
ALHA 77257 | | | | Goodrich et al. (1987b), Goodrich and Berkley (1986), Berkley and Jones (1982) | low | S2-S3 | meteorite find | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | based on the locale, region, or nearby town in which the fall occurred | Fo% 85 | can be severe due to long exposure time to environmental corrosion agents | | | large, anhedral olivine and pyroxene grains | lower because the fall was not witnessed | 485755 kg | | carbon, metal, sulfides small silicate grains along grain boundaries less than 10% by volume | in degrees, minutes and seconds of lattitude and longitude | | when the meteorite was found | | | | meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal | 1691 | less than 20 GPa | | 0 % | Wo% 6.8 En% 80 | curved meeting in triple junctions | 1 mm | 0.16 in modal pyroxene/(pryroxene+olivine) | |
ALHA 78262 | | | | Goodrich et al. (1987b), Goodrich and Berkley (1986), Berkley and Jones (1982) | low | S2-S3 | meteorite find | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | based on the locale, region, or nearby town in which the fall occurred | Fo% 78 | can be severe due to long exposure time to environmental corrosion agents | | | large, anhedral olivine and pyroxene grains | lower because the fall was not witnessed | 485755 kg | | carbon, metal, sulfides small silicate grains along grain boundaries less than 10% by volume | in degrees, minutes and seconds of lattitude and longitude | | when the meteorite was found | | | | meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal | 1691 | less than 20 GPa | | 0 % | Wo% 8.4 En% 72 | curved meeting in triple junctions | 1 mm | | |
Asuka 881931 | | | | Yanai and Kojima (1995b) | low | S2-S3 | meteorite find | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | based on the locale, region, or nearby town in which the fall occurred | Fo% 76 | can be severe due to long exposure time to environmental corrosion agents | | | large, anhedral olivine and pyroxene grains | lower because the fall was not witnessed | 485755 kg | | carbon, metal, sulfides small silicate grains along grain boundaries less than 10% by volume | in degrees, minutes and seconds of lattitude and longitude | | when the meteorite was found | | | | meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal | 1691 | less than 20 GPa | | 0 % | Wo% 8.8 En% 73 | curved meeting in triple junctions | 1 mm | | |
DaG 319 | | | | | unshocked | S1 | S1 shock stage meteorite | | Dar al Gani plateau, Libyan Sahara Desert | DaG 319 | | can be severe due to long exposure time to environmental corrosion agents | W2 | DaG | | lower because the fall was not witnessed | 9 kg (out of date) | bre - chia | smaller mineral fragments, carbon, suessite (Fe3Si), sulfides, minor chromite and minor apatite | 27° 01.68' N., 16° 21.52' E. | | 1997 | 0.740 kg |
 | | meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal | 6 (out of date) | less than 5 GPa | typical monomict ureilite material plus a variety of other lithic clasts | common in clasts | | | | | |
EET 87511 | EET 87717 meteorite | | | Berkley (1990), AMN 11-2 | low | S2-S3 | meteorite find | Wo% 4.5 En% 82 | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | based on the locale, region, or nearby town in which the fall occurred | Fo% 85 | can be severe due to long exposure time to environmental corrosion agents | | | bi-modal with extremely large 15mm crystals of low-Ca pyroxene poikilitically enclosing domains with ureilite texture | lower because the fall was not witnessed | 485755 kg | | carbon, metal, sulfides small silicate grains along grain boundaries less than 10% by volume | in degrees, minutes and seconds of lattitude and longitude | | when the meteorite was found | | | Wo% 36 En% 55 | meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal | 1691 | less than 20 GPa | | | | | | | |
EET 87517 | | | | AMN 11-2 | low | S2-S3 | meteorite find | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | based on the locale, region, or nearby town in which the fall occurred | Fo% 92 | can be severe due to long exposure time to environmental corrosion agents | | | large, anhedral olivine and pyroxene grains | lower because the fall was not witnessed | 485755 kg | | carbon, metal, sulfides small silicate grains along grain boundaries less than 10% by volume | in degrees, minutes and seconds of lattitude and longitude | | when the meteorite was found | | | | meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal | 1691 | less than 20 GPa | | 0 % | Wo% 5.0 En% 87 | curved meeting in triple junctions | 1 mm | 0.5 in modal pyroxene/(pryroxene+olivine) | |
LEW 85328 | | | | AMN 10-1 | low | S2-S3 | meteorite find | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | based on the locale, region, or nearby town in which the fall occurred | Fo% 80 | can be severe due to long exposure time to environmental corrosion agents | | | large, anhedral olivine and pyroxene grains | lower because the fall was not witnessed | 485755 kg | | carbon, metal, sulfides small silicate grains along grain boundaries less than 10% by volume | in degrees, minutes and seconds of lattitude and longitude | | when the meteorite was found | | | | meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal | 1691 | less than 20 GPa | | 0 % | Wo% 9.0 En% 74 | curved meeting in triple junctions | 1 mm | 0.33 in modal pyroxene/(pryroxene+olivine) | |
LEW 88006 | | | | AMN 13-2 | low | S2-S3 | meteorite find | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | based on the locale, region, or nearby town in which the fall occurred | Fo% 82 | can be severe due to long exposure time to environmental corrosion agents | | | large, anhedral olivine and pyroxene grains | lower because the fall was not witnessed | 485755 kg | | carbon, metal, sulfides small silicate grains along grain boundaries less than 10% by volume | in degrees, minutes and seconds of lattitude and longitude | | when the meteorite was found | | | | meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal | 1691 | less than 20 GPa | | 0 % | Wo% 8.0 En% 76 | curved meeting in triple junctions | 1 mm | | |
monomict-poikilitic ureilite | | small rounded pyroxene grains (poikilitic) | | | low | S2-S3 | | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | based on the locale, region, or nearby town in which the fall occurred | | | | | large, anhedral olivine and pyroxene grains | | 9 kg (out of date) | | carbon, metal, sulfides small silicate grains along grain boundaries less than 10% by volume | in degrees, minutes and seconds of lattitude and longitude | low shock ureilite | | | | | asteroid | 6 (out of date) | less than 20 GPa | | 0 % | | curved meeting in triple junctions | 1 mm | | small rounded olivine grains (poikilitic) |
Roosevelt County 027 | | | | Goodrich et al. (1987a) | low | S2-S3 | meteorite find | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | based on the locale, region, or nearby town in which the fall occurred | Fo% 79 | can be severe due to long exposure time to environmental corrosion agents | | | large, anhedral olivine and pyroxene grains | lower because the fall was not witnessed | 485755 kg | | carbon, metal, sulfides small silicate grains along grain boundaries less than 10% by volume | in degrees, minutes and seconds of lattitude and longitude | | when the meteorite was found | | | | meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal | 1691 | less than 20 GPa | | 0 % | Wo% 8.0 En% 75 | curved meeting in triple junctions | 1 mm | 0.25 in modal pyroxene/(pryroxene+olivine) | |
Y-74659 | | | | Takeda et al. (1979a), Takeda (1987), Takeda and Yanai (1978) | low | S2-S3 | meteorite find | Wo% 4.5 En% 88 | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | based on the locale, region, or nearby town in which the fall occurred | Fo% 91 | can be severe due to long exposure time to environmental corrosion agents | | | large, anhedral olivine and pyroxene grains | lower because the fall was not witnessed | 485755 kg | | carbon, metal, sulfides small silicate grains along grain boundaries less than 10% by volume | in degrees, minutes and seconds of lattitude and longitude | | when the meteorite was found | | | | meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal | 1691 | less than 20 GPa | | 0 % | Wo% 7.3 En% 86 | curved meeting in triple junctions | 1 mm | 0.52 in modal pyroxene/(pryroxene+olivine) | |
Y-791538 | | | | Yanai and Kojima (1995b), Takeda et al. (1992), Takeda (1989) | low | S2-S3 | meteorite find | Wo% 4.9 En% 88 | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | based on the locale, region, or nearby town in which the fall occurred | Fo% 91 | can be severe due to long exposure time to environmental corrosion agents | | | large, anhedral olivine and pyroxene grains | lower because the fall was not witnessed | 485755 kg | | carbon, metal, sulfides small silicate grains along grain boundaries less than 10% by volume | in degrees, minutes and seconds of lattitude and longitude | | when the meteorite was found | | | | meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal | 1691 | less than 20 GPa | | 0 % | Wo% 9.0 En% 84 | curved meeting in triple junctions | 1 mm | 0.45 in modal pyroxene/(pryroxene+olivine) | |
Y-82100 | | | | Yanai and Kojima (1995b) | low | S2-S3 | meteorite find | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | based on the locale, region, or nearby town in which the fall occurred | Fo% 81 | can be severe due to long exposure time to environmental corrosion agents | | | large, anhedral olivine and pyroxene grains | lower because the fall was not witnessed | 485755 kg | | carbon, metal, sulfides small silicate grains along grain boundaries less than 10% by volume | in degrees, minutes and seconds of lattitude and longitude | | when the meteorite was found | | | | meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal | 1691 | less than 20 GPa | | 0 % | Wo% 8.6 En% 77 | curved meeting in triple junctions | 1 mm | 0.2 in modal pyroxene/(pryroxene+olivine) | |
Y-8448 | | | | Yanai and Kojima (1995b) | low | S2-S3 | meteorite find | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | based on the locale, region, or nearby town in which the fall occurred | Fo% 78 | can be severe due to long exposure time to environmental corrosion agents | | | large, anhedral olivine and pyroxene grains | lower because the fall was not witnessed | 485755 kg | | carbon, metal, sulfides small silicate grains along grain boundaries less than 10% by volume | in degrees, minutes and seconds of lattitude and longitude | | when the meteorite was found | | | | meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal | 1691 | less than 20 GPa | | 0 % | variable | curved meeting in triple junctions | 1 mm | | |