PCA 82506 | is an instance of monomict-poikilitic ureilite |  |
is an instance of meteorite find |  |
has olivine composition Fo% 78 |  |
has pigeonite composition Wo% 6.0 En% 76 |  |
has pyroxene content 0.48 in modal pyroxene/(pryroxene+olivine) |  |
has reference Goodrich et al. (1987b), Berkley (1986) |  |
monomict-poikilitic ureilite | has olivine inclusions small rounded pyroxene grains (poikilitic) |  |
has pyroxene inclusions small rounded olivine grains (poikilitic) |  |
meteorite find | has find date when the meteorite was found |  |
has value lower because the fall was not witnessed |  |
has weathering can be severe due to long exposure time to environmental corrosion agents |  |
monomict ureilite | has texture large, anhedral olivine and pyroxene grains |  |
has intergranular boundary curved meeting in triple junctions |  |
has gain size 1 mm |  |
has plagioclase 0 % |  |
low shock ureilite | has shock stage S2-S3 |  |
has degree of shock metamorphism low |  |
has shock pressure less than 20 GPa |  |
has shock diagnostic mineral no diamonds or lonsdaleite |  |
has shock diagnostic mineral small euhedral graphite crystals can sometimes be distinguished |  |
has shock texture silicates show minor fracturing, undulatory extinction and kink bands primarily in olivine |  |
has olivine shock metamorphism fracturing, undulatory extinction and kink bands |  |
meteorite | has fall date recorded by eyewitness or inferred from dating methods |  |
has fall location strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity |  |
has fall coordinates in degrees, minutes and seconds of lattitude and longitude |  |
has fall map which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity |  |
can have crater image |  |
has original mass which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site |  |
has composition often minerals not found on Earth |  |
has relative abundance |  |
has total mass of finds 485755 kg |  |
has number of finds 1691 |  |
has impact velocity when it hits the ground which is smaller than its velocity before it enters the atmosphere |  |
has impact angle |  |
has weather resistance which depends on its composition |  |
has monetary value large if the fall was witnessed |  |
has name based on the locale, region, or nearby town in which the fall occurred |  |
often produce power outages and failures in electrical equipment due to EMP (electromagnetic pulse) |  |
can be associated with crater |  |
has origin meteoroid from interplanetary space or fragment dislodged from another planet, moon or planetesimal |  |
vaporizes completely if size is between 3 micrometers and 3 millimeters |  |
can survive fall if size is larger than 3 mm and velocity is less than 24 km per second |  |
can survive fall if it fragments because smaller pieces with less mass are more easily slowed by the atmosphere |  |
has ablative mass loss depending on composition, more friable stony meteoroids loses more mass than iron meteoroid |  |
has ablative mass loss directly proportional to initial velocity |  |
can shatter during impact phase |  |
can fragment during meteor phase |  |
has fragmentation probability during meteor phase which depends on composition |  |
ureilite | has letter designation AURE |  |
has characteristic mineral olivine-pigeonite about 90% by volume |  |
has matrix composition carbon, metal, sulfides small silicate grains along grain boundaries less than 10% by volume |  |
has minerology olivine, pyroxene (some combination of pigeonite, orthopyroxene, augite) |  |
has petrology coarse-grained granular |  |
has likely origin partial melting residue |  |
has olivine grain characteristic reduced rims contacting carbonaceous matrix material 0.1 mm FeO-free olivine and/or enstatite rims riddled with tiny inclusions of low-Ni metal |  |
rock | has part mineral |  |
has genesis |  |
shocked meteorite | has metamorphism mechanism shock metamorphism |  |
plutonic rock | has solidification mechanism cooling in deep underground chambers |  |
has solidification timescale very slow |  |
achondrite | has distinguishing feature no chondrules |  |