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shock melted meteorite comparison table
Subject has part mean Ni content of sulfide has solidification timescale has part carbon has olivine shock metamorphism has part matrix is independent of has shock pressure has matrix abundance has letter designation has pyroxene shock metamorphism has sediment mechanism has origin has likely origin has distinguishing feature has degree of secondary process has part feldspar has metal abundance has refractory inclusion abundance has solidification mechanism has chondrule mean diameter has petrology has chondrule glass type has age has original texture has number of find has part water has orthopyroxene shock metamorphism has plagioclase shock metamorphism has characteristic mineral has peak temperature has shock diagnostic mineral be shock has part metal maximum bulk has homogeneity of olivine and low Ca pyroxene has gain size has structural state of low Ca pyroxene has matrix composition has minerology has total mass of find has chondrule abundance has parent body has part chondrule has texture has olivine grain characteristic has petrologic type range
mosaicized ureilite very slow completely shattered or mosaicized  100 GPa or greater AUREmottled by melt glass asteroidpartial melting residueno chondrules    cooling in deep underground chambers coarse-grained granular  visible via dark matrix outlining relict grain boundaries of large, elongate grains, and a common preferred orientation of grains within relict domains -has source: Berkley JL, Taylor GJ, Keil K. Harlow GE, Prinz M 1980, Geochim Cosmochim Acta 44, 1579 -has URL: http://adsabs.harvard.edu/cgi-bin/bib_query?1980GeCoA..44.1579B6 (out of date)   olivine-pigeonite about 90% by volume diamonds and/or lonsdaleite   much less than 1 mm carbon, metal, sulfides small silicate grains along grain boundaries less than 10% by volumeolivine, pyroxene (some combination of pigeonite, orthopyroxene, augite)9 kg (out of date)   mosaicizedreduced rims contacting carbonaceous matrix material 0.1 mm FeO-free olivine and/or enstatite rims riddled with tiny inclusions of low-Ni metal 
shock melted chondritein weight % in weight %impact melt and melt brecciasfine grained disequilibrium mixture of silicates, oxides, metal, sulfides and organic constituentsthe nature and degree of thermal metamorphism or aqueous alterationgreater than 90 GPain volume %  agglomeration of particles, many of which record individual, diverse historiesmeteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal  providing insight into geological evolution of parent asteroidusually plagioclase tectosilicatein volume %in volume % millimeters  oldest and most primitive rock in solar system 1691in weight %impact melt and melt brecciasimpact melt and melt breccias less than 950 degree Celsius during its entire history since solidificationorthopyroxene for enstatite chondritebefore, during or after other types of metamorphismin weight %definition goes here definition goes here  485755 kgin volume %asteroid smaller than 100 km in diametersmall sphere of about 1 mm diameter of formerly melted minerals  which depends on degree of aqueous alteration and thermal metamorphism

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