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rock > meteorite > meteorite find > Sahara meteorite > Dar al Gani meteorite > UK 43
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UK 43 comparison table
Subject has sediment mechanism has weather resistance has metal abundance has part mean Ni content of sulfide has number of fragment has age has refractory inclusion abundance is an instance of has distinguishing feature has olivine and low Ca pyroxene homogeneity has part feldspar has fragmentation probability has part metal maximum bulk has distribution ellipse has fall location has chondrule glass type has weather has homogeneity of olivine and low Ca pyroxene has acronym has chondrule abundance has relative abundance has part chondrule has abundance has prototype has degree of aqueous alteration 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 matrix abundance has petrologic type range has part carbon has petrologic type has part maximum bulk Ni in metal is a kind of has find date has part water has mass has image has number of find has ablative mass loss classified by has chondrule mean diameter has part sulfide Ni content
CO chondriteagglomeration of particles, many of which record individual, diverse historieslow1 to 5 % by volumein weight % oldest and most primitive rock in solar system13 % by volume elemental carbongreater than 5 % deviationsminor primary grains onlyhigh because it is more friable than iron meteoritein weight % strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocityclear, isotropic, variable abundance definition goes here 48 % by volume8 % of meteorite fallschondrules very sharply definedrare relative to other chondrite typesOrnans meteoritenone 2577 kgpredominantly monoclinicless than 950 degree Celsius during its entire history since solidificationclastic and minor opaqueasteroid smaller than 100 km in diameternone34 % by volumewhich depends on degree of aqueous alteration and thermal metamorphism0.2 to 1 % by weight3greater than 20 % by weight, kamacite and taenite in exsolution relationshiptype 3 chondrite 0.3 to 3 % by weight  36high because it is more friable than iron meteorite 0.15 millimetersless than 0.5 % by weight
Dar al Gani meteorite which depends on its composition         during meteor phase which depends on composition  Dar al Gani plateau, Libyan Sahara Desert can be severe due to long exposure time to environmental corrosion agents DaG      lower because the fall was not witnessed485755 kg          Sahara meteoritewhen the meteorite was found   1691directly proportional to initial velocity   
UK 43agglomeration of particles, many of which record individual, diverse historieswhich depends on its composition1 to 5 % by volumein weight %2000 or moreoldest and most primitive rock in solar system13 % by volumeCO chondriteelemental carbongreater than 5 % deviationsminor primary grains onlyduring meteor phase which depends on compositionin weight %
Dar al Gani plateau, Libyan Sahara Desertclear, isotropic, variable abundancecan be severe due to long exposure time to environmental corrosion agentsdefinition goes hereDaG48 % by volume8 % of meteorite fallschondrules very sharply definedrare relative to other chondrite typesOrnans meteoritenonelower because the fall was not witnessed2577 kgpredominantly monoclinicless than 950 degree Celsius during its entire history since solidificationclastic and minor opaqueasteroid smaller than 100 km in diameternone34 % by volumewhich depends on degree of aqueous alteration and thermal metamorphism0.2 to 1 % by weight3greater than 20 % by weight, kamacite and taenite in exsolution relationship 19990.3 to 3 % by weight177 kg
36directly proportional to initial velocityOpen University, UK. Meteoritical Bulletin No 840.15 millimetersless than 0.5 % by weight

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