Subject |
has reference |
has minerology |
has degree of shock metamorphism |
has shock stage |
is an instance of |
has distinguishing feature |
has olivine grain characteristic |
has fall date |
has metamorphism mechanism |
has pyroxene shock metamorphism |
has likely origin |
has solidification mechanism |
has shock diagnostic mineral |
has olivine composition |
has olivine shock metamorphism |
has fall description |
has weather |
has letter designation |
has texture |
has value |
has total mass of find |
has matrix composition |
has characteristic mineral |
is a kind of |
has original texture |
has number of find |
has origin |
has shock pressure |
has solidification timescale |
has pigeonite composition |
has definition |
has gain size |
has pyroxene content |
has petrology |
meteorite fall | | | | | | | | recorded by eyewitness or instruments | | | | | | | | what witnesses saw or what was recorded by instruments | negligible due to quick recovery of meteorite before corrosion begins | | | higher because the fall was witnessed | 485755 kg | | | meteorite | | 1691 | meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal | | | | a meteorite whose fall was witnessed by human or electronic means | | | |
mosaicized ureilite | | olivine, pyroxene (some combination of pigeonite, orthopyroxene, augite) | shock melted | shock melted | | no chondrules | reduced rims contacting carbonaceous matrix material 0.1 mm FeO-free olivine and/or enstatite rims riddled with tiny inclusions of low-Ni metal | recorded by eyewitness or inferred from dating methods | shock metamorphism | mottled by melt glass | partial melting residue | cooling in deep underground chambers | diamonds and/or lonsdaleite | | completely shattered or mosaicized | | | AURE | mosaicized | | 9 kg (out of date) | carbon, metal, sulfides small silicate grains along grain boundaries less than 10% by volume | olivine-pigeonite about 90% by volume | shock melted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M 1980, Geochim Cosmochim Acta 44, 1579 -has URL: http://adsabs.harvard.edu/cgi-bin/bib_query?1980GeCoA..44.1579B | 6 (out of date) | asteroid | 100 GPa or greater | very slow | | | much less than 1 mm | | coarse-grained granular |
Dyalpur | Berkley et. al (1980) | olivine, pyroxene (some combination of pigeonite, orthopyroxene, augite) | shock melted | shock melted | meteorite fall | no chondrules | reduced rims contacting carbonaceous matrix material 0.1 mm FeO-free olivine and/or enstatite rims riddled with tiny inclusions of low-Ni metal | recorded by eyewitness or instruments | shock metamorphism | mottled by melt glass | partial melting residue | cooling in deep underground chambers | diamonds and/or lonsdaleite | Fo% 84 | completely shattered or mosaicized | what witnesses saw or what was recorded by instruments | negligible due to quick recovery of meteorite before corrosion begins | AURE | mosaicized | higher because the fall was witnessed | 485755 kg | carbon, metal, sulfides small silicate grains along grain boundaries less than 10% by volume | olivine-pigeonite about 90% by volume | | 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 | 1691 | meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal | 100 GPa or greater | very slow | Wo% 11 En% 76 | | much less than 1 mm | 0.41 in modal pyroxene/(pryroxene+olivine) | coarse-grained granular |