Subject |
has sediment mechanism |
has metal abundance |
has part mean Ni content of sulfide |
has minerology |
has age |
has refractory inclusion abundance |
is an instance of |
has distinguishing feature |
has olivine and low Ca pyroxene homogeneity |
has part feldspar |
has part metal maximum bulk |
has fall location |
has likely origin |
has solidification mechanism |
has name |
has chondrule glass type |
has letter designation |
has homogeneity of olivine and low Ca pyroxene |
has chondrule abundance |
has relative abundance |
has part chondrule |
has abundance |
has prototype |
has degree of aqueous alteration |
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 characteristic mineral |
has petrologic type |
has part maximum bulk Ni in metal |
has composition |
is a kind of |
has find date |
has part water |
has image |
has origin |
has number of find |
has solidification timescale |
has chondrule mean diameter |
has part sulfide Ni content |
be an acronym for |
has petrology |
CK3 chondrite | agglomeration of particles, many of which record individual, diverse histories | 0.01 % by volume | in weight % | | oldest and most primitive rock in solar system | 4 % by volume | | elemental carbon | greater than 5 % deviations | minor primary grains only | in weight % | 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 | clear, isotropic, variable abundance | | definition goes here | 15 % by volume | 8 % of meteorite falls | chondrules very sharply defined | rare relative to other chondrite types | ??? 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 | 75 % 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 | often minerals not found on Earth | type 3 chondrite | | 0.3 to 3 % by weight | | meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal | 36 | | 0.7 millimeters | less than 0.5 % by weight | | |
eucrite | | | | orthopyroxene, olivine, chromite; pigeonite, calcic plagioclase, silica | | | | no chondrules | | | | 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 | based on the locale, region, or nearby town in which the fall occurred | | AUEC | | | 7.1 % of meteorite falls | | | | | 231 kg | | | | | | | | | anorthite-pigeonite Ca-rich | | | silicates (with very few exceptions) | basalt | | | | 4 Vesta | 23 | very rapid | | | Howardite, Eucrite, Diogenite | coarse-grained orthopyroxenites, gabbros, fine- to coarse-grained basalts, brecciated |
Camel Donga 003 | agglomeration of particles, many of which record individual, diverse histories | 0.01 % by volume | in weight % | orthopyroxene, olivine, chromite; pigeonite, calcic plagioclase, silica | oldest and most primitive rock in solar system | 4 % by volume | eucrite | elemental carbon | greater than 5 % deviations | minor primary grains only | in weight % | Camel Donga, West Australia, Australia | cumulates, crystallized melts, impact mixing | extrusion onto the surface of the planet or asteroid via a volcanic eruption | Camel Donga | clear, isotropic, variable abundance | AUEC | definition goes here | 15 % by volume | 8 % of meteorite falls | chondrules very sharply defined | rare relative to other chondrite types | ??? meteorite | none | 231 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 | 75 % by volume | which depends on degree of aqueous alteration and thermal metamorphism | 0.2 to 1 % by weight | anorthite-pigeonite Ca-rich | 3 | greater than 20 % by weight, kamacite and taenite in exsolution relationship | silicates (with very few exceptions) | | 1984 | 0.3 to 3 % by weight |
 | 4 Vesta | 23 | very rapid | 0.7 millimeters | less than 0.5 % by weight | Howardite, Eucrite, Diogenite | coarse-grained orthopyroxenites, gabbros, fine- to coarse-grained basalts, brecciated |