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 witnessed | 485755 kg | | in degrees, minutes and seconds of lattitude and longitude | | Sahara meteorite | when the meteorite was found | | | | 1691 | meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal | | | | | |
mosaicized ureilite | | olivine, pyroxene (some combination of pigeonite, orthopyroxene, augite) | shock melted | shock melted | | no chondrules | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | reduced rims contacting carbonaceous matrix material 0.1 mm FeO-free olivine and/or enstatite rims riddled with tiny inclusions of low-Ni metal | shock metamorphism | mottled by melt glass | partial melting residue | cooling in deep underground chambers | based on the locale, region, or nearby town in which the fall occurred | diamonds and/or lonsdaleite | | completely shattered or mosaicized | | | AURE | | mosaicized | | 9 kg (out of date) | carbon, metal, sulfides small silicate grains along grain boundaries less than 10% by volume | in degrees, minutes and seconds of lattitude and longitude | olivine-pigeonite about 90% by volume | shock 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..44.1579B | 6 (out of date) | asteroid | 100 GPa or greater | very slow | | much less than 1 mm | coarse-grained granular |
DaG 084 | Weber and Bischoff (1996) | olivine, pyroxene (some combination of pigeonite, orthopyroxene, augite) | shock melted | shock melted | Dar al Gani meteorite | no chondrules | Dar al Gani plateau, Libyan Sahara Desert | reduced rims contacting carbonaceous matrix material 0.1 mm FeO-free olivine and/or enstatite rims riddled with tiny inclusions of low-Ni metal | shock metamorphism | mottled by melt glass | partial melting residue | cooling in deep underground chambers | DaG 084 | diamonds and/or lonsdaleite | Fo% 79 | completely shattered or mosaicized | can be severe due to long exposure time to environmental corrosion agents | W3 | AURE | DaG | mosaicized | lower because the fall was not witnessed | 9 kg (out of date) | carbon, metal, sulfides small silicate grains along grain boundaries less than 10% by volume | 27° 02.44' N., 16° 24.26' E. | olivine-pigeonite about 90% by volume | | 1995 | 0.277 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..44.1579B | 6 (out of date) | meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal | 100 GPa or greater | very slow | Wo% 5.0 En% 81 | much less than 1 mm | coarse-grained granular |