Subject |
has iron metal and iron sulfide |
has sediment mechanism |
has weather resistance |
has metal abundance |
has part mean Ni content of sulfide |
has age |
has refractory inclusion abundance |
is an instance of |
has total iron content |
has olivine and low Ca pyroxene homogeneity |
has part feldspar |
has fragmentation probability |
has metal iron content |
has part metal maximum bulk |
has fall location |
has name |
has chondrule glass type |
has weather |
has homogeneity of olivine and low Ca pyroxene |
has chondrule abundance |
has relative abundance |
has part chondrule |
has abundance |
has degree of aqueous alteration |
has value |
has total mass of find |
has structural state of low Ca pyroxene |
has peak temperature |
has parent body |
has part matrix |
has degree of thermal metamorphism |
has fall coordinate |
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 comment |
has find date |
has part water |
has mass |
has image |
has number of find |
has ablative mass loss |
has synonym |
has definition |
has chondrule mean diameter |
has part sulfide Ni content |
H3 chondrite | 75 % of total iron | agglomeration of particles, many of which record individual, diverse histories | low | 10 % by volume | in weight % | oldest and most primitive rock in solar system | 0.1 to 1 % by volume | | high | greater than 5 % deviations | minor primary grains only | high because it is more friable than iron meteorite | 12 to 21 % | 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 | 60 to 80 % by volume | 85.7 % of meteorite falls | chondrules very sharply defined | most common chondrite observed from falls | none | | 349 kg | predominantly monoclinic | less than 950 degree Celsius during its entire history since solidification | asteroid smaller than 100 km in diameter | clastic and minor opaque | none | in degrees, minutes and seconds of lattitude and longitude | 10 to 15 % 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 | | | 9 | high because it is more friable than iron meteorite | bronzite chondrite | | 0.3 millimeters | less than 0.5 % by weight |
meteorite find | | | which depends on its composition | | | | | | | | | during meteor phase which depends on composition | | | 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 | | can be severe due to long exposure time to environmental corrosion agents | | | | | | | lower because the fall was not witnessed | 485755 kg | | | | | | in degrees, minutes and seconds of lattitude and longitude | | | | | | meteorite | | when the meteorite was found | | | | 1691 | directly proportional to initial velocity | | a meteorite whose fall was not witnessed | | |
Abbott | 75 % of total iron | agglomeration of particles, many of which record individual, diverse histories | which depends on its composition | 10 % by volume | in weight % | oldest and most primitive rock in solar system | 0.1 to 1 % by volume | meteorite find | high | greater than 5 % deviations | minor primary grains only | during meteor phase which depends on composition | 12 to 21 % | in weight % | Colfax County, New Mexico | Abbott | clear, isotropic, variable abundance | can be severe due to long exposure time to environmental corrosion agents | definition goes here | 60 to 80 % by volume | | chondrules very sharply defined | most common chondrite observed from falls | none | lower because the fall was not witnessed | 349 kg | predominantly monoclinic | less than 950 degree Celsius during its entire history since solidification | asteroid smaller than 100 km in diameter | clastic and minor opaque | none | 36° 18' N., 104° 17' W. | 10 to 15 % 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 | | polymict regolith breccia | 1951 | 0.3 to 3 % by weight | 9.5 kg |
 | 9 | directly proportional to initial velocity | bronzite chondrite | | 0.3 millimeters | less than 0.5 % by weight |