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 acronym |
has matrix abundance |
has sediment mechanism |
has olivine composition |
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 weathering stage |
is a kind of |
has age |
has number of fragment |
has part sulfide Ni content |
has part maximum bulk Ni in metal |
has total iron content |
has number of find |
has petrologic type |
has find date |
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 |
be shock |
has fall location |
is an instance of |
has pyroxene composition |
has shock stage |
has part metal maximum bulk |
has homogeneity of olivine and low Ca pyroxene |
has composition |
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 |
classified by |
has petrologic type range |
Dar al Gani meteorite | | which depends on its composition | | | | | | | | DaG | | | | | can be severe due to long exposure time to environmental corrosion agents | | | | | | during meteor phase which depends on composition | | | | Sahara meteorite | | | | | | 1691 | | when the meteorite was found | | | | | | | | | | | | Dar al Gani plateau, Libyan Sahara Desert | | | | | | often minerals not found on Earth | | lower because the fall was not witnessed | in degrees, minutes and seconds of lattitude and longitude | | directly proportional to initial velocity | 485755 kg | | | | | | |
LL5 chondrite | in weight % | low | less than 0.2 % by weight | amphoterite | 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 | 2 % by volume | 0.1 to 1 % by volume | 85.7 % of meteorite falls | high because it is more friable than iron meteorite | 0.9 millimeters | thermal metamorphism | | type 5 chondrite | 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 | low | 9 | 5 | | less than 1.5 % by weight | moderate | | | 20 % of total iron | | | most common chondrite observed from falls | less than 950 degree Celsius during its entire history since solidification | | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | | | | in weight % | definition goes here | bronzite, olivine and minor oligoclase | less than 20 % monoclinic | | in degrees, minutes and seconds of lattitude and longitude | homogeneous | high because it is more friable than iron meteorite | 184 kg | 60 to 80 % by volume | asteroid smaller than 100 km in diameter | chondrules readily delineated | about 2 % | | which depends on degree of aqueous alteration and thermal metamorphism |
S3 shock stage chondrite | in weight % | which depends on its composition | in weight % | | | planar fractures, undulatory extinction, irregular fractures | fine grained disequilibrium mixture of silicates, oxides, metal, sulfides and organic constituents | the nature and degree of thermal metamorphism or aqueous alteration | 15 to 20 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 | | S3 shock stage meteorite | oldest and most primitive rock in solar system | | | | | 1691 | | | in weight % | | clinoenstatite lamellae on (100), undulatory extinction, planar fractures, irregular fractures | undulatory extinction | | weakly shocked | | | less than 950 degree Celsius during its entire history since solidification | orthopyroxene for enstatite chondrite | before, during or after other types of metamorphism | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | | | S3 | in weight % | definition goes here | often minerals not found on Earth | 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 |
DaG 639 | in weight % | which depends on its composition | less than 0.2 % by weight | amphoterite | the range over at which the alteration took place | planar fractures, undulatory extinction, irregular fractures | transparent, recrystallized, moderate size crystals | the nature and degree of thermal metamorphism or aqueous alteration | 15 to 20 GPa | DaG | 10 to 15 % by volume | agglomeration of particles, many of which record individual, diverse histories | Fa% 26.8 |
 | can be severe due to long exposure time to environmental corrosion agents | providing insight into geological evolution of parent asteroid | secondary, 2 to 50 micron grains | 2 % by volume | 0.1 to 1 % by volume | | during meteor phase which depends on composition | 0.9 millimeters | thermal metamorphism | W2 | | oldest and most primitive rock in solar system | 1 | less than 0.5 % by weight | greater than 20 % by weight, kamacite and taenite in exsolution relationship | low | 9 | 5 | 1998 | less than 1.5 % by weight | moderate | clinoenstatite lamellae on (100), undulatory extinction, planar fractures, irregular fractures | undulatory extinction | 20 % of total iron | weakly shocked | 0.237 kg | most common chondrite observed from falls | less than 950 degree Celsius during its entire history since solidification | orthopyroxene for enstatite chondrite | before, during or after other types of metamorphism | Dar al Gani plateau, Libyan Sahara Desert | LL5 chondrite | Fs% 22.1 | S3 | in weight % | definition goes here | bronzite, olivine and minor oligoclase | less than 20 % monoclinic | lower because the fall was not witnessed | 26° 56.41' N. 16° 25.14' E. | homogeneous | directly proportional to initial velocity | 184 kg | 60 to 80 % by volume | asteroid smaller than 100 km in diameter | chondrules readily delineated | about 2 % | A. Sexton, Open University, UK. Meteoritical Bulletin No 84 | which depends on degree of aqueous alteration and thermal metamorphism |