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rock > igneous rock > differentiated meteorite > differentiated achondrite > asteroidal achondrite > ureilite > mosaicized ureilite > DaG 084
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DaG 084 comparison table
Subject has reference has minerology has degree of shock metamorphism has shock stage is an instance of has distinguishing feature has fall location has olivine grain characteristic has metamorphism mechanism has pyroxene shock metamorphism has likely origin has solidification mechanism has name has shock diagnostic mineral has olivine composition has olivine shock metamorphism has weather has weathering stage has letter designation has acronym has texture has value has total mass of find has matrix composition has fall coordinate has characteristic mineral is a kind of has find date has mass has image has original texture has number of find has origin has shock pressure has solidification timescale has pigeonite composition has gain size has petrology
Dar al Gani meteorite      Dar al Gani plateau, Libyan Sahara Desert     based on the locale, region, or nearby town in which the fall occurred   can be severe due to long exposure time to environmental corrosion agents  DaG lower because the fall was not witnessed485755 kg in degrees, minutes and seconds of lattitude and longitude Sahara meteoritewhen the meteorite was found   1691meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal     
mosaicized ureilite olivine, pyroxene (some combination of pigeonite, orthopyroxene, augite)shock meltedshock melted no chondrulesstrewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocityreduced rims contacting carbonaceous matrix material 0.1 mm FeO-free olivine and/or enstatite rims riddled with tiny inclusions of low-Ni metalshock metamorphismmottled by melt glasspartial melting residuecooling in deep underground chambersbased on the locale, region, or nearby town in which the fall occurreddiamonds and/or lonsdaleite completely shattered or mosaicized  AURE mosaicized 9 kg (out of date)carbon, metal, sulfides small silicate grains along grain boundaries less than 10% by volumein degrees, minutes and seconds of lattitude and longitudeolivine-pigeonite about 90% by volumeshock melted meteorite   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)asteroid100 GPa or greatervery slow much less than 1 mmcoarse-grained granular
DaG 084Weber and Bischoff (1996)olivine, pyroxene (some combination of pigeonite, orthopyroxene, augite)shock meltedshock meltedDar al Gani meteoriteno chondrulesDar al Gani plateau, Libyan Sahara Desertreduced rims contacting carbonaceous matrix material 0.1 mm FeO-free olivine and/or enstatite rims riddled with tiny inclusions of low-Ni metalshock metamorphismmottled by melt glasspartial melting residuecooling in deep underground chambersDaG 084diamonds and/or lonsdaleiteFo% 79completely shattered or mosaicizedcan be severe due to long exposure time to environmental corrosion agentsW3AUREDaGmosaicizedlower because the fall was not witnessed9 kg (out of date)carbon, metal, sulfides small silicate grains along grain boundaries less than 10% by volume27° 02.44' N., 16° 24.26' E.olivine-pigeonite about 90% by volume 19950.277 kg
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)meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal100 GPa or greatervery slowWo% 5.0 En% 81much less than 1 mmcoarse-grained granular

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