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rock > metamorphic rock > altered chondrite > thermally altered chondrite > type 4 chondrite > LL4 chondrite > Soko Banja
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Soko Banja comparison table
Subject has iron metal and iron sulfide has sediment mechanism has weather resistance has metal abundance has part mean Ni content of sulfide has alteration temperature range 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 fall date has metamorphism mechanism has degree of secondary process 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 abundance 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 has composition is a kind of 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
LL4 chondrite20 % of total ironagglomeration of particles, many of which record individual, diverse historieslow2 % by volumein weight %the range over at which the alteration took placeoldest and most primitive rock in solar system0.1 to 1 % by volume lowless than 5 % mean deviationssecondary, grains than 2 micronshigh because it is more friable than iron meteoriteabout 2 %in weight %strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocityrecorded by eyewitness or inferred from dating methodsthermal metamorphismproviding insight into geological evolution of parent asteroidbased on the locale, region, or nearby town in which the fall occurreddevitrified, absent  definition goes here60 to 80 % by volume85.7 % of meteorite fallschondrules well definedmost common chondrite observed from falls 124 kggreater than 20 % monoclinicless than 950 degree Celsius during its entire history since solidificationasteroid smaller than 100 km in diametertransparent, recrystallized, small crystalsweakin degrees, minutes and seconds of lattitude and longitude10 to 15 % by volumewhich depends on degree of aqueous alteration and thermal metamorphismless than 0.2 % by weight4greater than 20 % by weight, kamacite and taenite in exsolution relationshipbronzite, olivine and minor oligoclasetype 4 chondriteless than 1.5 % by weight  2high because it is more friable than iron meteoriteamphoterite 0.9 millimetersless 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 velocityrecorded 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 beginswhat witnesses saw or what was recorded by instruments     higher because the fall was witnessed485755 kg     in degrees, minutes and seconds of lattitude and longitude     often minerals not found on Earthmeteorite   1691directly proportional to initial velocity a meteorite whose fall was witnessed by human or electronic means  
Soko Banja20 % of total ironagglomeration of particles, many of which record individual, diverse historieswhich depends on its composition2 % by volumein weight %the range over at which the alteration took placeoldest and most primitive rock in solar system0.1 to 1 % by volumemeteorite falllowless than 5 % mean deviationssecondary, grains than 2 micronsduring meteor phase which depends on compositionabout 2 %in weight %Serbia, YugoslaviaOctober 13, 1877thermal metamorphismproviding insight into geological evolution of parent asteroidSoko Banjadevitrified, absentnegligible due to quick recovery of meteorite before corrosion beginswhat witnesses saw or what was recorded by instrumentsdefinition goes here60 to 80 % by volume chondrules well definedmost common chondrite observed from fallshigher because the fall was witnessed124 kggreater than 20 % monoclinicless than 950 degree Celsius during its entire history since solidificationasteroid smaller than 100 km in diametertransparent, recrystallized, small crystalsweak43° 40' N., 21° 52' E.10 to 15 % by volumewhich depends on degree of aqueous alteration and thermal metamorphismless than 0.2 % by weight4greater than 20 % by weight, kamacite and taenite in exsolution relationshipoften minerals not found on Earth less than 1.5 % by weight80 kg
2directly proportional to initial velocityamphoterite 0.9 millimetersless than 0.5 % by weight

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