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Mundrabilla comparison table |
Subject | has part mean Ni content of sulfide | has weather resistance | has part carbon | has daubreelite | has part matrix | has mafic mineral | has prototype | has nickel content | has iridium content | has chr | has degree of aqueous alteration | has matrix abundance | has phosphor content | has sediment mechanism | has origin | has gallium content | has image | has distinguishing feature | has part feldspar | has metal abundance | has refractory inclusion abundance | has relative abundance | has fragmentation probability | has chondrule mean diameter | have composition | has arsenic content | is a kind of | has chondrule glass type | has age | has part sulfide Ni content | has part maximum bulk Ni in metal | has copper content | has troilite | has structural class | has number of find | has antimony content | has petrologic type | has find date | has part water | has plagioclase | has degree of thermal metamorphism | has abundance | has metal | has peak temperature | has tungsten content | has W.P. | has name | has crystal size | has fall location | is an instance of | has chromium content | parent body radiu | has formation cooling rate | has schreibersite | has cobalt content | has cohenite | has palladium content | has part metal maximum bulk | has germanium content | has molydbenum content | has homogeneity of olivine and low Ca pyroxene | has gold content | has graphite | has composition | has structural state of low Ca pyroxene | has metal content | has fall coordinate | has olivine and low Ca pyroxene homogeneity | has ablative mass loss | has total mass of find | has chondrule abundance | has parent body | has part chondrule | has petrologic type range |
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CV chondrite | in weight % | low | 0.2 to 1 % by weight | clastic and minor opaque | Vigarano meteorite | weak | 40 % by volume | agglomeration of particles, many of which record individual, diverse histories | meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal | elemental carbon | minor primary grains only | 0 to 5 % by volume | 10 % by volume | 8 % of meteorite falls | high because it is more friable than iron meteorite | 1.0 millimeters | type 3 chondrite | clear, isotropic, variable abundance | oldest and most primitive rock in solar system | less than 0.5 % by weight | greater than 20 % by weight, kamacite and taenite in exsolution relationship | 36 | 3 | 0.3 to 3 % by weight | none | rare relative to other chondrite types | less than 950 degree Celsius during its entire history since solidification | based on the locale, region, or nearby town in which the fall occurred | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | in weight % | definition goes here | iron-rich olivine, calcium aluminum inclusions | predominantly monoclinic | in degrees, minutes and seconds of lattitude and longitude | greater than 5 % deviations | high because it is more friable than iron meteorite | 2577 kg | 45 % by volume | asteroid smaller than 100 km in diameter | chondrules very sharply defined | which depends on degree of aqueous alteration and thermal metamorphism | |||||||||||||||||||||||||||||||||
Of octahedrite | high | always greater than 4 % | planet or asteroid much larger than 100 km in diameter | crystalline iron-nickel alloy | 5.7 % of meteorite falls | low because it is tougher than stony meteorite | octahedrite | Of | 532 | based on the locale, region, or nearby town in which the fall occurred | 0.2 to 0.5 mm (fine) | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | silicates (with very few exceptions) | higher than that of average solar system material | in degrees, minutes and seconds of lattitude and longitude | low because it has higher tensile strength than stony meteorite | 454624 kg | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||
sulfide-rich IAB iron | high | % by volume | includes olivine, orthopyroxene and clinopyroxene in % by volume | Mundrabilla meteorite | 6.4 % by weight | 2.7 microgram/gram | % by volume | 2.1 milligram/gram | asteroid wide partial melting | 96 microgram/gram | 5.7 % of meteorite falls | low because it is tougher than stony meteorite | 11 microgram/gram | type IAB iron meteorite | 132 microgram/gram | % by volume | 532 | 270 nanogram/gram | % by volume | % by volume | 1.6 microgram/gram | % by volume | based on the locale, region, or nearby town in which the fall occurred | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | 16 microgram/gram | 33 kilometers | 25 degrees C per million years | % by volume | 4.6 milligram/gram | % by volume | 3.5 microgram/gram | 400 microgram/gram | 8.2 microgram/gram | 1.5 microgram/gram | % by volume | high in troilite | higher than that of average solar system material | in degrees, minutes and seconds of lattitude and longitude | low because it has higher tensile strength than stony meteorite | 454624 kg | ||||||||||||||||||||||||||||||||||
Mundrabilla | in weight % | low | 0.2 to 1 % by weight | 1.6 % by volume | clastic and minor opaque | 48.5 % by volume | Vigarano meteorite | 7.47 % by weight | 2.7 microgram/gram | % by volume | weak | 40 % by volume | 2.1 milligram/gram | agglomeration of particles, many of which record individual, diverse histories | asteroid wide partial melting | 96 microgram/gram | elemental carbon | minor primary grains only | 0 to 5 % by volume | 10 % by volume | 8 % of meteorite falls | high because it is more friable than iron meteorite | 1.0 millimeters | 7.72% Ni, 59.5 ppm Ga, 196 ppm Ge, 0.87 ppm Ir | 11 microgram/gram | clear, isotropic, variable abundance | oldest and most primitive rock in solar system | less than 0.5 % by weight | greater than 20 % by weight, kamacite and taenite in exsolution relationship | 132 microgram/gram | 30.5 % by volume | Of | 36 | 270 nanogram/gram | 3 | 1911 | 0.3 to 3 % by weight | 14.9 % by volume | none | rare relative to other chondrite types | 0.12 % by volume | less than 950 degree Celsius during its entire history since solidification | 1.6 microgram/gram | 0.69 % by volume | Mundrabilla | 0.6 mm (fine) | Mundrabilla, Nullarbor Plain, Western Australia | CV chondrite | 16 microgram/gram | 33 kilometers | 25 degrees C per million years | % by volume | 4.6 milligram/gram | % by volume | 3.5 microgram/gram | in weight % | 400 microgram/gram | 8.2 microgram/gram | definition goes here | 1.5 microgram/gram | 3.7 % by volume | iron-rich olivine, calcium aluminum inclusions | predominantly monoclinic | higher than that of average solar system material | Latitude 30 degrees 47 minutes South, Longitude 127 degrees 33 minutes East | greater than 5 % deviations | high because it is more friable than iron meteorite | 2577 kg | 45 % by volume | asteroid smaller than 100 km in diameter | chondrules very sharply defined | which depends on degree of aqueous alteration and thermal metamorphism |
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