Subject |
has part mean Ni content of sulfide |
has weather resistance |
has part carbon |
has synonym |
has alteration temperature range |
has olivine shock metamorphism |
has part matrix |
is independent of |
has shock pressure |
has matrix abundance |
has sediment mechanism |
has image |
has weather |
has degree of secondary process |
has part feldspar |
has metal abundance |
has refractory inclusion abundance |
has relative abundance |
has fragmentation probability |
has chondrule mean diameter |
has metamorphism mechanism |
has fall date |
has fall description |
is a kind of |
has chondrule glass type |
has age |
has part sulfide Ni content |
has part maximum bulk Ni in metal |
has total iron content |
has definition |
has number of find |
has petrologic type |
has part water |
has degree of thermal metamorphism |
has orthopyroxene shock metamorphism |
has plagioclase shock metamorphism |
has iron metal and iron sulfide |
has degree of shock metamorphism |
has mass |
has abundance |
has peak temperature |
has shock diagnostic mineral |
has name |
be shock |
has fall location |
is an instance of |
has shock stage |
has part metal maximum bulk |
has homogeneity of olivine and low Ca pyroxene |
has structural state of low Ca pyroxene |
has value |
has fall coordinate |
has olivine and low Ca pyroxene homogeneity |
has ablative mass loss |
has total mass of find |
has chondrule abundance |
has parent body |
has part chondrule |
has metal iron content |
has petrologic type range |
H5 chondrite | in weight % | low | less than 0.2 % by weight | bronzite chondrite | the range over at which the alteration took place | | transparent, recrystallized, moderate size crystals | | | 10 to 15 % by volume | agglomeration of particles, many of which record individual, diverse histories | | | providing insight into geological evolution of parent asteroid | secondary, 2 to 50 micron grains | 10 % by volume | 0.1 to 1 % by volume | 85.7 % of meteorite falls | high because it is more friable than iron meteorite | 0.3 millimeters | thermal metamorphism | recorded by eyewitness or inferred from dating methods | | type 5 chondrite | devitrified, absent | oldest and most primitive rock in solar system | less than 0.5 % by weight | greater than 20 % by weight, kamacite and taenite in exsolution relationship | high | | 76 | 5 | less than 1.5 % by weight | moderate | | | 75 % of total iron | | | most common chondrite observed from falls | less than 950 degree Celsius during its entire history since solidification | | based on the locale, region, or nearby town in which the fall occurred | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | | | in weight % | definition goes here | less than 20 % monoclinic | | in degrees, minutes and seconds of lattitude and longitude | homogeneous | high because it is more friable than iron meteorite | 1267 kg | 60 to 80 % by volume | asteroid smaller than 100 km in diameter | chondrules readily delineated | 12 to 21 % | which depends on degree of aqueous alteration and thermal metamorphism |
meteorite fall | | which depends on its composition | | | | | | | | | | | negligible due to quick recovery of meteorite before corrosion begins | | | | | | during meteor phase which depends on composition | | | recorded by eyewitness or instruments | what witnesses saw or what was recorded by instruments | meteorite | | | | | | a meteorite whose fall was witnessed by human or electronic means | 1691 | | | | | | | | | | | | based on the locale, region, or nearby town in which the fall occurred | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | | | | | | higher because the fall was witnessed | in degrees, minutes and seconds of lattitude and longitude | | directly proportional to initial velocity | 485755 kg | | | | | |
S4 shock stage chondrite | in weight % | which depends on its composition | in weight % | | | weak mosaicism, planar fractures | fine grained disequilibrium mixture of silicates, oxides, metal, sulfides and organic constituents | the nature and degree of thermal metamorphism or aqueous alteration | 30 to 35 GPa | in volume % | agglomeration of particles, many of which record individual, diverse histories | | | providing insight into geological evolution of parent asteroid | usually plagioclase tectosilicate | in volume % | in volume % | | during meteor phase which depends on composition | millimeters | shock metamorphism | recorded by eyewitness or inferred from dating methods | | S4 shock stage meteorite | | oldest and most primitive rock in solar system | | | | | 1691 | | in weight % | | weak mosaicism, twinning on (100), planar fractures | undulatory extinction, partially isotropic, planar deformation features | | moderately shocked | | | less than 950 degree Celsius during its entire history since solidification | orthopyroxene for enstatite chondrite | based on the locale, region, or nearby town in which the fall occurred | before, during or after other types of metamorphism | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | | S4 | in weight % | definition goes here | definition goes here | | in degrees, minutes and seconds of lattitude and longitude | | directly proportional to initial velocity | 485755 kg | in volume % | asteroid smaller than 100 km in diameter | small sphere of about 1 mm diameter of formerly melted minerals | | which depends on degree of aqueous alteration and thermal metamorphism |
Monahans (1998) | in weight % | which depends on its composition | less than 0.2 % by weight | bronzite chondrite | the range over at which the alteration took place | weak mosaicism, planar fractures | transparent, recrystallized, moderate size crystals | the nature and degree of thermal metamorphism or aqueous alteration | 30 to 35 GPa | 10 to 15 % by volume | agglomeration of particles, many of which record individual, diverse histories |
 | negligible due to quick recovery of meteorite before corrosion begins | providing insight into geological evolution of parent asteroid | secondary, 2 to 50 micron grains | 10 % by volume | 0.1 to 1 % by volume | | during meteor phase which depends on composition | 0.3 millimeters | shock metamorphism | 6:47 pm March 22, 1998 | what witnesses saw or what was recorded by instruments | | devitrified, absent | oldest and most primitive rock in solar system | less than 0.5 % by weight | greater than 20 % by weight, kamacite and taenite in exsolution relationship | high | | 76 | 5 | less than 1.5 % by weight | moderate | weak mosaicism, twinning on (100), planar fractures | undulatory extinction, partially isotropic, planar deformation features | 75 % of total iron | moderately shocked | 2.587 kg | most common chondrite observed from falls | less than 950 degree Celsius during its entire history since solidification | orthopyroxene for enstatite chondrite | Monahans (1998) | before, during or after other types of metamorphism | Allen Street, Monahans, Texas | S4 shock stage chondrite | S4 | in weight % | definition goes here | less than 20 % monoclinic | higher because the fall was witnessed | 102° 53.5' W., 31° 36.5' N. | homogeneous | directly proportional to initial velocity | 1267 kg | 60 to 80 % by volume | asteroid smaller than 100 km in diameter | chondrules readily delineated | 12 to 21 % | which depends on degree of aqueous alteration and thermal metamorphism |