Subject |
has sediment mechanism |
has weather resistance |
has metal abundance |
has part mean Ni content of sulfide |
has number of fragment |
has age |
has refractory inclusion abundance |
is an instance of |
has distinguishing feature |
has olivine and low Ca pyroxene homogeneity |
has part feldspar |
has fragmentation probability |
has part metal maximum bulk |
has distribution ellipse |
has fall location |
has chondrule glass type |
has weather |
has homogeneity of olivine and low Ca pyroxene |
has acronym |
has chondrule abundance |
has relative abundance |
has part chondrule |
has abundance |
has prototype |
has degree of aqueous alteration |
has value |
has total mass of find |
has structural state of low Ca pyroxene |
has peak temperature |
has part matrix |
has parent body |
has degree of thermal metamorphism |
has matrix abundance |
has petrologic type range |
has part carbon |
has petrologic type |
has part maximum bulk Ni in metal |
is a kind of |
has find date |
has part water |
has mass |
has image |
has number of find |
has ablative mass loss |
classified by |
has chondrule mean diameter |
has part sulfide Ni content |
CO chondrite | agglomeration of particles, many of which record individual, diverse histories | low | 1 to 5 % by volume | in weight % | | oldest and most primitive rock in solar system | 13 % by volume | | elemental carbon | greater than 5 % deviations | minor primary grains only | high because it is more friable than iron meteorite | in weight % | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | clear, isotropic, variable abundance | | definition goes here | | 48 % by volume | 8 % of meteorite falls | chondrules very sharply defined | rare relative to other chondrite types | Ornans meteorite | none | | 2577 kg | predominantly monoclinic | less than 950 degree Celsius during its entire history since solidification | clastic and minor opaque | asteroid smaller than 100 km in diameter | none | 34 % by volume | which depends on degree of aqueous alteration and thermal metamorphism | 0.2 to 1 % by weight | 3 | greater than 20 % by weight, kamacite and taenite in exsolution relationship | type 3 chondrite | | 0.3 to 3 % by weight | | | 36 | high because it is more friable than iron meteorite | | 0.15 millimeters | less than 0.5 % by weight |
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 | | | | | | | | | | | Sahara meteorite | when the meteorite was found | | | | 1691 | directly proportional to initial velocity | | | |
UK 43 | agglomeration of particles, many of which record individual, diverse histories | which depends on its composition | 1 to 5 % by volume | in weight % | 2000 or more | oldest and most primitive rock in solar system | 13 % by volume | CO chondrite | elemental carbon | greater than 5 % deviations | minor primary grains only | during meteor phase which depends on composition | in weight % |
 | Dar al Gani plateau, Libyan Sahara Desert | clear, isotropic, variable abundance | can be severe due to long exposure time to environmental corrosion agents | definition goes here | DaG | 48 % by volume | 8 % of meteorite falls | chondrules very sharply defined | rare relative to other chondrite types | Ornans meteorite | none | lower because the fall was not witnessed | 2577 kg | predominantly monoclinic | less than 950 degree Celsius during its entire history since solidification | clastic and minor opaque | asteroid smaller than 100 km in diameter | none | 34 % by volume | which depends on degree of aqueous alteration and thermal metamorphism | 0.2 to 1 % by weight | 3 | greater than 20 % by weight, kamacite and taenite in exsolution relationship | | 1999 | 0.3 to 3 % by weight | 177 kg |
 | 36 | directly proportional to initial velocity | Open University, UK. Meteoritical Bulletin No 84 | 0.15 millimeters | less than 0.5 % by weight |