Subject |
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 olivine and low Ca pyroxene homogeneity |
has part feldspar |
has fragmentation probability |
has part metal maximum bulk |
has fall location |
has fall date |
has name |
has chondrule glass type |
has weather |
has fall description |
has homogeneity of olivine and low Ca pyroxene |
has chondrule abundance |
has relative abundance |
has part chondrule |
has prototype |
has degree of aqueous alteration |
has petrologic subtype |
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 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 part water |
has image |
has number of find |
has ablative mass loss |
has definition |
has chondrule mean diameter |
has part sulfide Ni content |
K chondrite | agglomeration of particles, many of which record individual, diverse histories | low | 0 % by volume (included in matrix abundance) | in weight % | oldest and most primitive rock in solar system | less than 0.1 % by volume | | 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 | recorded by eyewitness or inferred from dating methods | based on the locale, region, or nearby town in which the fall occurred | clear, isotropic, variable abundance | | | definition goes here | 27 % by volume | 85.7 % of meteorite falls | chondrules very sharply defined | Kakangari meteorite | none | | | 20461 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 | in degrees, minutes and seconds of lattitude and longitude | 73 % by volume (including metal) | 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 | | 1030 | high because it is more friable than iron meteorite | | 0.6 millimeters | less than 0.5 % by weight |
meteorite fall | | 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 | recorded by eyewitness or instruments | based on the locale, region, or nearby town in which the fall occurred | | negligible due to quick recovery of meteorite before corrosion begins | what witnesses saw or what was recorded by instruments | | | | | | | | higher because the fall was witnessed | 485755 kg | | | | | | in degrees, minutes and seconds of lattitude and longitude | | | | | | meteorite | | | 1691 | directly proportional to initial velocity | a meteorite whose fall was witnessed by human or electronic means | | |
Kakangari | agglomeration of particles, many of which record individual, diverse histories | which depends on its composition | 0 % by volume (included in matrix abundance) | in weight % | oldest and most primitive rock in solar system | less than 0.1 % by volume | meteorite fall | greater than 5 % deviations | minor primary grains only | during meteor phase which depends on composition | in weight % | Kangankarai, India | June 4, 1890 | Kakangari | clear, isotropic, variable abundance | negligible due to quick recovery of meteorite before corrosion begins | what witnesses saw or what was recorded by instruments | definition goes here | 27 % by volume | | chondrules very sharply defined | Kakangari meteorite | none | 3.6 | higher because the fall was witnessed | 485755 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 | 12° 23' N., 78° 31' E. | 73 % by volume (including metal) | 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 | | 0.3 to 3 % by weight |
 | 1691 | directly proportional to initial velocity | | 0.6 millimeters | less than 0.5 % by weight |