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 distinguishing feature |
has part feldspar |
has part metal maximum bulk |
has fragmentation probability |
has fall location |
has fall date |
has name |
has chondrule glass type |
has fall description |
has weather |
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 petrologic subtype |
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 petrologic type range |
has matrix abundance |
has fall coordinate |
has part carbon |
has petrologic type |
has part maximum bulk Ni in metal |
has composition |
has original mass |
is a kind of |
has part water |
has image |
has number of find |
have composition |
has ablative mass loss |
has synonym |
has definition |
has chondrule mean diameter |
has part sulfide Ni content |
has fall map |
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 | | what witnesses saw or what was recorded by instruments | negligible due to quick recovery of meteorite before corrosion begins | | | | | | | | | higher because the fall was witnessed | 485755 kg | | | | | | | | in degrees, minutes and seconds of lattitude and longitude | | | | often minerals not found on Earth | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | meteorite | | | 1691 | | directly proportional to initial velocity | | a meteorite whose fall was witnessed by human or electronic means | | | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity |
oxidized-Allende subgroup CV chondrite | agglomeration of particles, many of which record individual, diverse histories | low | 0 to 5 % by volume | in weight % | oldest and most primitive rock in solar system | 10 % by volume | | greater than 5 % deviations | elemental carbon | minor primary grains only | in weight % | high because it is more friable than iron meteorite | 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 | 45 % by volume | 8 % of meteorite falls | chondrules very sharply defined | rare relative to other chondrite types | Allende meteorite | weak | | | 2577 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 | which depends on degree of aqueous alteration and thermal metamorphism | 40 % by volume | in degrees, minutes and seconds of lattitude and longitude | 0.2 to 1 % by weight | 3 | greater than 20 % by weight, kamacite and taenite in exsolution relationship | iron-rich olivine, calcium aluminum inclusions | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | CV chondrite | 0.3 to 3 % by weight | | 36 | | high because it is more friable than iron meteorite | CV3OxA chondrite | | 1.0 millimeters | less than 0.5 % by weight | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity |
Allende | agglomeration of particles, many of which record individual, diverse histories | which depends on its composition | 0 to 5 % by volume | in weight % | oldest and most primitive rock in solar system | 10 % by volume | meteorite fall | greater than 5 % deviations | elemental carbon | minor primary grains only | in weight % | during meteor phase which depends on composition | village of Pueblito de Allende, Chihuahua State, Mexico | February 8, 1969 1:05 am | Allende | clear, isotropic, variable abundance | what witnesses saw or what was recorded by instruments | negligible due to quick recovery of meteorite before corrosion begins | definition goes here | 45 % by volume | | chondrules very sharply defined | rare relative to other chondrite types | Allende meteorite | weak | 3.2 | higher because the fall was witnessed | 485755 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 | which depends on degree of aqueous alteration and thermal metamorphism | 40 % by volume | 26° 58' N., 105° 19' W. | 0.2 to 1 % by weight | 3 | greater than 20 % by weight, kamacite and taenite in exsolution relationship | often minerals not found on Earth | several tons | | 0.3 to 3 % by weight |
 | 1691 | iron rich olivine matrix, 24 % iron, rare flecks of iron-nickel | directly proportional to initial velocity | CV3OxA chondrite | | 1.0 millimeters | less than 0.5 % by weight |
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