PAT 91546 | is an instance of CH chondrite |  |
CH chondrite | has prototype ALH 85085 meteorite |  |
has chondrule abundance about 70 % by volume |  |
has matrix abundance 5 % by volume |  |
has refractory inclusion abundance 0.1 % by volume |  |
has metal abundance 20 % by volume |  |
has chondrule mean diameter 0.02 millimeters |  |
has volatile content low |  |
carbonaceous chondrite | has relative abundance 8 % of meteorite falls |  |
has total mass of finds 2577 kg |  |
has number of finds 36 |  |
has distinguishing feature elemental carbon |  |
has abundance rare relative to other chondrite types |  |
type 3 chondrite | has petrologic type 3 |  |
has degree of aqueous alteration none |  |
has degree of thermal metamorphism none |  |
has olivine and low Ca pyroxene homogeneity greater than 5 % deviations |  |
has structural state of low Ca pyroxene predominantly monoclinic |  |
has chondrule glass type clear, isotropic, variable abundance |  |
has part feldspar minor primary grains only |  |
has part maximum bulk Ni in metal greater than 20 % by weight, kamacite and taenite in exsolution relationship |  |
has part sulfide Ni content less than 0.5 % by weight |  |
has part matrix clastic and minor opaque |  |
has part chondrule chondrules very sharply defined |  |
has part carbon 0.2 to 1 % by weight |  |
has part water 0.3 to 3 % by weight |  |
chondrite | has petrologic type range which depends on degree of aqueous alteration and thermal metamorphism |  |
has homogeneity of olivine and low Ca pyroxene definition goes here |  |
has part metal maximum bulk in weight % |  |
has part mean Ni content of sulfides in weight % |  |
stony meteorite | has weather resistance low |  |
has fragmentation probability high because it is more friable than iron meteorite |  |
has ablative mass loss high because it is more friable than iron meteorite |  |
undifferentiated meteorite | has peak temperature less than 950 degree Celsius during its entire history since solidification |  |
has parent body asteroid smaller than 100 km in diameter |  |
has age oldest and most primitive rock in solar system |  |
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 impact velocity when it hits the ground which is smaller than its velocity before it enters the atmosphere |  |
has impact angle |  |
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 |  |
can shatter during impact phase |  |
can fragment during meteor phase |  |
conglomerate | has sediment mechanism agglomeration of particles, many of which record individual, diverse histories |  |
rock | has part mineral |  |
has texture |  |
has genesis |  |