Subject |
has part mean Ni content of sulfide |
has part carbon |
has synonym |
has alteration temperature range |
has olivine shock metamorphism |
has part matrix |
has prototype |
is independent of |
has nickel content |
has shock pressure |
has olivine content |
has degree of aqueous alteration |
has matrix abundance |
has shock texture |
has letter designation |
has pyroxene shock metamorphism |
has petrologic subtype |
has sediment mechanism |
has likely origin |
has olivine composition |
has pigeonite composition |
has image |
has distinguishing feature |
has degree of secondary process |
has part feldspar |
has metal abundance |
has olivine composition uniformity |
has refractory inclusion abundance |
has relative abundance |
has minor mineral |
has oxidized iron content |
has chondrule mean diameter |
has petrology |
has intergranular boundary |
has metamorphism mechanism |
has fall date |
has original mass |
have composition |
has chromite content |
has chondrule glass type |
has age |
has part sulfide Ni content |
has part maximum bulk Ni in metal |
has oxidation state |
has troilite content |
has original texture |
has olivine crystal distribution |
has total iron content |
has number of find |
has volatile content |
has petrologic type |
has part water |
has comment |
has plagioclase |
has orthopyroxene shock metamorphism |
has plagioclase shock metamorphism |
has iron metal and iron sulfide |
has degree of thermal metamorphism |
has probability of occurence |
has characteristic mineral |
has degree of shock metamorphism |
has olivine grain size |
has schreibersite content |
has mass |
has abundance |
has peak temperature |
has property |
has phosphate content |
has shock diagnostic mineral |
has name |
be shock |
has fall location |
is an instance of |
has reference |
has pyroxene content |
parent body radiu |
has tenacity |
has formation cooling rate |
has olivine grain shape |
has shock stage |
has shape |
has part metal maximum bulk |
be an acronym for |
has homogeneity of olivine and low Ca pyroxene |
has curatorial location |
has gain size |
has composition |
has structural state of low Ca pyroxene |
has matrix composition |
has metal content |
has minerology |
has fall coordinate |
has olivine and low Ca pyroxene homogeneity |
has total mass of find |
has fall map |
has chondrule abundance |
has parent body |
has part chondrule |
has metal iron content |
has texture |
has olivine grain characteristic |
has petrologic type range |
Abee | in weight % | less than 0.2 % by weight | E chondrite | the range over at which the alteration took place | | transparent, recrystallized, small crystals | | | | | | | less than 2 to 15 % by volume | | | | | agglomeration of particles, many of which record individual, diverse histories | | | |
 | | providing insight into geological evolution of parent asteroid | secondary, grains than 2 microns | 8 % by volume | | 0.1 to 1 % by volume | | | zero | 0.2 millimeters | | | thermal metamorphism | 11:05 pm June 9, 1952 | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | 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 | highly reduced with very little FeO | | | | high | 1691 | | 3 to 5 | less than 1.5 % by weight | melt breccia | | | | | weak | | | | | | 107 kg | | less than 950 degree Celsius during its entire history since solidification | | | | Abee | | Abee, Alberta | meteorite fall | | | | | | | | | in weight % | | definition goes here | | | often minerals not found on Earth | greater than 20 % monoclinic | | | | 54° 13' N., 113° 0' W. | less than 5 % mean deviations | 485755 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | 60 to 80 % by volume | asteroid smaller than 100 km in diameter | chondrules well defined | | | | which depends on degree of aqueous alteration and thermal metamorphism |
Allende | in weight % | 0.2 to 1 % by weight | CV3OxA chondrite | | | clastic and minor opaque | Allende meteorite | | | | | weak | 40 % by volume | | | | 3.2 | agglomeration of particles, many of which record individual, diverse histories | | | |
 | elemental carbon | | minor primary grains only | 0 to 5 % by volume | | 10 % by volume | | | | 1.0 millimeters | | | | February 8, 1969 1:05 am | several tons | iron rich olivine matrix, 24 % iron, rare flecks of iron-nickel | | clear, isotropic, variable abundance | 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 | | | | | | 1691 | | 3 | 0.3 to 3 % by weight | | | | | | none | | | | | | | rare relative to other chondrite types | less than 950 degree Celsius during its entire history since solidification | | | | Allende | | village of Pueblito de Allende, Chihuahua State, Mexico | meteorite fall | | | | | | | | | in weight % | | definition goes here | | | often minerals not found on Earth | predominantly monoclinic | | | | 26° 58' N., 105° 19' W. | greater than 5 % deviations | 485755 kg |
 | 45 % by volume | asteroid smaller than 100 km in diameter | chondrules very sharply defined | | | | which depends on degree of aqueous alteration and thermal metamorphism |
Angra dos Reis | | | | | | | Angra dos Reis meteorite | | | | | | | | ACANOM | | | | crystallized melts, cumulates (?) | | |
 | no chondrules | | | | | | | | | | fine- to coarse-grained igneous | | | 5:00 am January 20, 1869 | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | | | | | | | | | | 1691 | | | | | | | | | | | augite | | | | 1.5 kg | | | | | | Angra dos Reis | | Rio de Janeiro, Brazil | meteorite fall | | | | | | | | | | | | | | often minerals not found on Earth | | | | Al-Ti-diopside, anorthite, calcic olivine | 22° 58' S., 44° 19' W. | | 485755 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | | | | | | | |
Bilanga | | | | | | | | | | | | | | | ADIO | | | | cumulates, crystallized melts, impact mixing | | |
 | no chondrules | | | | | | | | | | coarse-grained orthopyroxenites, gabbros, fine- to coarse-grained basalts, brecciated | | | 10:30 am October 27, 1999 | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | | | | | | | | | | 8 | | | | | | | | | | higher for non-spherical, flattened or angular meteoroids | hyperstene | | | | 25 kg | | | formed by separation of molten rock in a gravity field | | | Bilanga | | Bilanga Yanga and Gomponsago, Burkina Faso, Africa | oriented meteorite | | | | | | | | conical from preferential ablation during atmospheric passage | | Howardite, Eucrite, Diogenite | | | | often minerals not found on Earth | | | | orthopyroxene, olivine, chromite; pigeonite, calcic plagioclase, silica | 12° 27' N., 0° 05' W. | | 68 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | | | | | | | |
Bruderheim | in weight % | less than 0.2 % by weight | hypersthene chondrite | the range over at which the alteration took place | | transparent, recrystallized, coarse 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, grains greater than 50 microns | 5 % by volume | | 0.1 to 1 % by volume | | | | 0.7 millimeters | | | thermal metamorphism | March 4, 1960 | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | 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 | | | | | low | 155 | | 6 | less than 1.5 % by weight | | | | | 50 % of total iron | strong | | | | | | 400 kg | most common chondrite observed from falls | less than 950 degree Celsius during its entire history since solidification | | | | Bruderheim | | Alberta, Canada | meteorite fall | | | | | | | | | in weight % | | definition goes here | | | often minerals not found on Earth | orthorhombic | | | | 53° 54' N., 112° 53' W. | homogeneous | 4673 kg |
 | 60 to 80 % by volume | asteroid smaller than 100 km in diameter | chondrules poorly defined | 5 to 10 % | | | which depends on degree of aqueous alteration and thermal metamorphism |
Dyalpur | | | | | completely shattered or mosaicized | | | | | 100 GPa or greater | | | | | AURE | mottled by melt glass | | | partial melting residue | Fo% 84 | Wo% 11 En% 76 | | no chondrules | | | | | | | | | | coarse-grained granular | | shock metamorphism | recorded by eyewitness or instruments | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | | | | | | | 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 | | | | | | | | | | | olivine-pigeonite about 90% by volume | shock melted | | | | | | | | diamonds and/or lonsdaleite | 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 | meteorite fall | Berkley et. al (1980) | 0.41 in modal pyroxene/(pryroxene+olivine) | | | | | shock melted | | | | | | much less than 1 mm | often minerals not found on Earth | | carbon, metal, sulfides small silicate grains along grain boundaries less than 10% by volume | | olivine, pyroxene (some combination of pigeonite, orthopyroxene, augite) | in degrees, minutes and seconds of lattitude and longitude | | 485755 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | | | | | mosaicized | reduced rims contacting carbonaceous matrix material 0.1 mm FeO-free olivine and/or enstatite rims riddled with tiny inclusions of low-Ni metal | |
Grosnaja | in weight % | 0.2 to 1 % by weight | CV3OxB chondrite | | planar fractures, undulatory extinction, irregular fractures | clastic and minor opaque | Bali meteorite | the nature and degree of thermal metamorphism or aqueous alteration | | 15 to 20 GPa | | weak | 40 % by volume | | | | 3.3 | agglomeration of particles, many of which record individual, diverse histories | | | |
 | elemental carbon | providing insight into geological evolution of parent asteroid | minor primary grains only | 0 to 5 % by volume | | 10 % by volume | | | | 1.0 millimeters | | | shock metamorphism | June 28, 1861 7:00 pm | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | clear, isotropic, variable abundance | 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 | | | | | | 1691 | | 3 | 0.3 to 3 % by weight | | | clinoenstatite lamellae on (100), undulatory extinction, planar fractures, irregular fractures | undulatory extinction | | none | | | weakly shocked | | | 3.5 kg | rare relative to other chondrite types | less than 950 degree Celsius during its entire history since solidification | | | orthopyroxene for enstatite chondrite | Grosnaja | before, during or after other types of metamorphism | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | S3 shock stage chondrite | | | | | | | S3 | | in weight % | | definition goes here | | | often minerals not found on Earth | predominantly monoclinic | | | | 43° 40' N., 45° 23' E. | greater than 5 % deviations | 485755 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | 45 % by volume | asteroid smaller than 100 km in diameter | chondrules very sharply defined | | | | which depends on degree of aqueous alteration and thermal metamorphism |
Havero | | | | | completely shattered or mosaicized | | | | | 100 GPa or greater | | | | | AURE | mottled by melt glass | | | partial melting residue | Fo% 79 | Wo% 2.5 En% 81 clinobronzite | | no chondrules | | | | | | | | | | coarse-grained granular | curved meeting in triple junctions | shock metamorphism | recorded by eyewitness or instruments | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | | | | | | | 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 | | | | | 0 % | | | | | | olivine-pigeonite about 90% by volume | shock melted | | | | | | | | diamonds and/or lonsdaleite | 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 | meteorite fall | Berkley et. al (1980) | 0.17 in modal pyroxene/(pryroxene+olivine) | | | | | shock melted | | | | | | much less than 1 mm | often minerals not found on Earth | | carbon, metal, sulfides small silicate grains along grain boundaries less than 10% by volume | | olivine, pyroxene (some combination of pigeonite, orthopyroxene, augite) | in degrees, minutes and seconds of lattitude and longitude | | 485755 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | | | | | mosaicized | reduced rims contacting carbonaceous matrix material 0.1 mm FeO-free olivine and/or enstatite rims riddled with tiny inclusions of low-Ni metal | |
Holbrook | in weight % | less than 0.2 % by weight | hypersthene chondrite | the range over at which the alteration took place | | transparent, recrystallized, coarse 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, grains greater than 50 microns | 5 % by volume | | 0.1 to 1 % by volume | | | | 0.7 millimeters | | | thermal metamorphism | 7:15 pm July 19, 1912 | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | 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 | | | | | low | 155 | | 6 | less than 1.5 % by weight | | | | | 50 % of total iron | strong | | | | | | 217.9 kg | most common chondrite observed from falls | less than 950 degree Celsius during its entire history since solidification | | | | Holbrook | | Navajo County, Arizona | meteorite fall | | | | | | | | | in weight % | | definition goes here | | | often minerals not found on Earth | orthorhombic | | | | 34° 54' N., 110° 11' W. | homogeneous | 4673 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | 60 to 80 % by volume | asteroid smaller than 100 km in diameter | chondrules poorly defined | 5 to 10 % | | | which depends on degree of aqueous alteration and thermal metamorphism |
Indarch | in weight % | less than 0.2 % by weight | E chondrite | the range over at which the alteration took place | planar fractures, undulatory extinction, irregular fractures | transparent, recrystallized, small crystals | | the nature and degree of thermal metamorphism or aqueous alteration | | 15 to 20 GPa | | | less than 2 to 15 % by volume | | | | | agglomeration of particles, many of which record individual, diverse histories | | | |
 | | providing insight into geological evolution of parent asteroid | secondary, grains than 2 microns | 8 % by volume | | 0.1 to 1 % by volume | | | zero | 0.2 millimeters | | | shock metamorphism | 8:10 pm April 7, 1891 | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | 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 | highly reduced with very little FeO | | | | high | 1691 | | 3 to 5 | less than 1.5 % by weight | | | clinoenstatite lamellae on (100), undulatory extinction, planar fractures, irregular fractures | undulatory extinction | | weak | | | weakly shocked | | | 27 kg | | less than 950 degree Celsius during its entire history since solidification | | | orthopyroxene for enstatite chondrite | Indarch | before, during or after other types of metamorphism | Azerbaydzhan SSR, USSR | S3 shock stage chondrite | | | | | | | S3 | | in weight % | | definition goes here | | | often minerals not found on Earth | greater than 20 % monoclinic | | | | 39° 45' N., 46° 40' E. | less than 5 % mean deviations | 485755 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | 60 to 80 % by volume | asteroid smaller than 100 km in diameter | chondrules well defined | | | | which depends on degree of aqueous alteration and thermal metamorphism |
Johnstown | | | | | | | | | | | | | | | ADIO | | | | cumulates, crystallized melts, impact mixing | | |
 | no chondrules | | | | | | | | | | coarse-grained orthopyroxenites, gabbros, fine- to coarse-grained basalts, brecciated | | | 4:20 pm July 6, 1924 | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | | | | | | | | | | 8 | | | | | | | | | | | hyperstene | | | | 40.3 kg | | | formed by separation of molten rock in a gravity field | | | Johnstown | | Weld County, Colorado | meteorite fall | | | | | | | | | | Howardite, Eucrite, Diogenite | | | | often minerals not found on Earth | | | | orthopyroxene, olivine, chromite; pigeonite, calcic plagioclase, silica | 40° 21' N., 104° 54' W. | | 68 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | | | | | | | |
Kakangari | in weight % | 0.2 to 1 % by weight | | | | clastic and minor opaque | Kakangari meteorite | | | | | none | 73 % by volume (including metal) | | | | 3.6 | agglomeration of particles, many of which record individual, diverse histories | | | |
 | | | minor primary grains only | 0 % by volume (included in matrix abundance) | | less than 0.1 % by volume | | | | 0.6 millimeters | | | | June 4, 1890 | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | clear, isotropic, variable abundance | 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 | | | | | | 1691 | | 3 | 0.3 to 3 % by weight | | | | | | none | | | | | | | | less than 950 degree Celsius during its entire history since solidification | | | | Kakangari | | Kangankarai, India | meteorite fall | | | | | | | | | in weight % | | definition goes here | | | often minerals not found on Earth | predominantly monoclinic | | | | 12° 23' N., 78° 31' E. | greater than 5 % deviations | 485755 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | 27 % by volume | asteroid smaller than 100 km in diameter | chondrules very sharply defined | | | | which depends on degree of aqueous alteration and thermal metamorphism |
Kapoeta | | | | | | | | | | | | | | | AHOW | | | | cumulates, crystallized melts, impact mixing | | |
 | no chondrules | | | | | | | | | | coarse-grained orthopyroxenites, gabbros, fine- to coarse-grained basalts, brecciated | | | 7:00 pm April 22, 1942 | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | | | | | | | | | | 19 | | | | | | | | | | | eucrite-diogenite mixture | | | | 11.355 kg | | | | | | Kapoeta | | Kapoeta-Nathalani Road, Equatoria, Sudan | meteorite fall | | | | | | | | | | Howardite, Eucrite, Diogenite | | | | often minerals not found on Earth | | | | orthopyroxene, olivine, chromite; pigeonite, calcic plagioclase, silica | 31° 10' S., 127° 45' E. | | 41 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | | | | | | | |
Lahrauli | | | | | sub-grain boundaries may be prominent | | | | | from 20 GPa to 100 GPa | | | | greater extent of fracturing, undulatory extinction, and kink banding | AURE | may be cloudy due to glassy inclusions | | | partial melting residue | Fo% 79 | Wo% 7.7 En% 74 | | no chondrules | | | | | | | | | | coarse-grained granular | curved meeting in triple junctions | shock metamorphism | recorded by eyewitness or instruments | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | | | | | | | | | | 1691 | | | | | 0 % | | | | | | olivine-pigeonite about 90% by volume | medium | | | | | | | | diamonds and/or lonsdaleite | 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 | meteorite fall | Malhotra (1962), Bhandari et al. (1981) | | | | | | S4-S6 | | | | | | 1 mm | often minerals not found on Earth | | carbon, metal, sulfides small silicate grains along grain boundaries less than 10% by volume | | olivine, pyroxene (some combination of pigeonite, orthopyroxene, augite) | in degrees, minutes and seconds of lattitude and longitude | | 485755 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | | | | | large, anhedral olivine and pyroxene grains | reduced rims contacting carbonaceous matrix material 0.1 mm FeO-free olivine and/or enstatite rims riddled with tiny inclusions of low-Ni metal | |
Lodran | | | | | | | Lodran meteorite | | | | | | | | LOD | | | agglomeration of particles, many of which record individual, diverse histories | ultrametamorphism, partial melting with some melt migration | | |
 | no chondrules | | | | | | | | | | fine- to coarse-grained equigranular | | | 2:00 pm October 1, 1868 | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | | oldest and most primitive rock in solar system | | | | | | | | 1691 | | | | | | | | | | | | | | | 1 kg | | less than 950 degree Celsius during its entire history since solidification | | | | Lodran | | 12 miles east of Lodhran, Pakistan | meteorite fall | | | | | | | | | | | | | | iron, pyroxene, olivine subcondritic abundances of plagioclase and troilite; | | | | olivine, orthopyroxene, clinopyroxene, metal with some troilite and some sodic plagioclase | 29° 32' N., 71° 48' E. | | 485755 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | | asteroid smaller than 100 km in diameter | | | coarse grained | | |
Marjalahti | | | | | | | | | always greater than 4 % | | 35 to 85 % by volume | | | | PAL | | | | | Fo 88+-1 | |
 | mixture of iron-nickel alloy and non-metallic minerals | | | | heterogeneous elements are zoned between grain rim and core | | | schreibersite | | | | | | 10:00 pm June 1, 1902 | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | 1 % or less by volume | | | | | | 0.1 to 7.3 % by volume | | from homogeneous to heterogeneous | | 33 | | | | | | | | | | | | | typically one centimeter | 0.3 to 2.8 % by volume | 45 kg | | | | 1 % or less by volume | | Marjalahti | | Lake Laatokka, Viipuri, Karelia, USSR (ASSR, Finland.) | main group pallasite | | | 78 to 97 kilometers | | 2.5 to 4 degrees C per million years | from angular fragments to rounded | | | | | | | | metallic iron plus olivine; core/mantle boundary samples | | | higher than that of average solar system material | | 61° 30' N., 30° 30' E. | | 7207 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | | | | | | | |
Mayo Belwa | | | | | | | | | | | | | | | AUB | | | | melted and crystallized residues from partial melting | | |
 | no chondrules | | | | | | | | | | breccias of igneous lithologies | | | August 3, 1974 | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | | | | | highly reduced with very little FeO | | | | | 9 | | | | | | | | | | | enstatite | | | | 4.85 kg | | | | | | Mayo Belwa | | Adamawa district of north-eastern Nigeria | meteorite fall | | | | | | | | | | | | | | often minerals not found on Earth | | | | enstatite, forsterite, sodic plagioclase, metal, numerous sulfides | 8° 58' N., 12° 5' E. | | 1205 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | | | | | | | |
Monahans (1998) | in weight % | 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 | | | |
 | | providing insight into geological evolution of parent asteroid | secondary, 2 to 50 micron grains | 10 % by volume | | 0.1 to 1 % by volume | | | | 0.3 millimeters | | | shock metamorphism | 6:47 pm March 22, 1998 | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | 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 | | | weak mosaicism, twinning on (100), planar fractures | undulatory extinction, partially isotropic, planar deformation features | 75 % of total iron | moderate | | | 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 | | | often minerals not found on Earth | less than 20 % monoclinic | | | | 102° 53.5' W., 31° 36.5' N. | homogeneous | 1267 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | 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 |
Mount Tazerzait | in weight % | less than 0.2 % by weight | hypersthene chondrite | the range over at which the alteration took place | sharp optical extinction, irregular fractures | transparent, recrystallized, moderate size crystals | | the nature and degree of thermal metamorphism or aqueous alteration | | less than 5 GPa | | | 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 | 5 % by volume | | 0.1 to 1 % by volume | | | | 0.7 millimeters | | | shock metamorphism | August 21, 1991 | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | 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 | | | | | low | 44 | | 5 | less than 1.5 % by weight | | | sharp optical extinction, irregular fractures | sharp optical extinction, irregular fractures | 50 % of total iron | moderate | | | unshocked | | | 110 kg | most common chondrite observed from falls | less than 950 degree Celsius during its entire history since solidification | | | orthopyroxene for enstatite chondrite | Mt. Tazerzait | before, during or after other types of metamorphism | Tahoua, Republic of Niger | S1 shock stage chondrite | | | | | | | S1 | | in weight % | | definition goes here | | | often minerals not found on Earth | less than 20 % monoclinic | | | | 18° 42' N., 4° 48' E. | homogeneous | 1256 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | 60 to 80 % by volume | asteroid smaller than 100 km in diameter | chondrules readily delineated | 5 to 10 % | | | which depends on degree of aqueous alteration and thermal metamorphism |
Murchison | in weight % | 0.8 to 2.6 % by weight | | | sharp optical extinction, irregular fractures | mostly fine, opaque | Mighei meteorite | the nature and degree of thermal metamorphism or aqueous alteration | | less than 5 GPa | | moderate | 70 % by volume | | | | | agglomeration of particles, many of which record individual, diverse histories | | | |
 | elemental carbon | providing insight into geological evolution of parent asteroid | minor primary grains only | 0.1 % by volume | | 5 % by volume | | | | 0.3 millimeters | | | shock metamorphism | September 28, 1969 10:45 am | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | contain amino acids | | rare | oldest and most primitive rock in solar system | greater than 0.5 % by weight | less than 20 % by weight; taenite minor or absent | | | | | | 1691 | | 2 | 2 to 16 % by weight | | | sharp optical extinction, irregular fractures | sharp optical extinction, irregular fractures | | | | | unshocked | | | | rare relative to other chondrite types | less than 950 degree Celsius during its entire history since solidification | | | orthopyroxene for enstatite chondrite | Murchison | before, during or after other types of metamorphism | Murchison, Victoria, Australia | S1 shock stage chondrite | | | | friable | | | S1 | | in weight % | | definition goes here | | | often minerals not found on Earth | predominantly monoclinic | | | | 36° 37' S., 145° 12' E. | greater than 5 % deviations | 485755 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | 20 % by volume | asteroid smaller than 100 km in diameter | chondrules very sharply defined | | | | which depends on degree of aqueous alteration and thermal metamorphism |
Ningqiang | in weight % | in weight % | | | | fine grained disequilibrium mixture of silicates, oxides, metal, sulfides and organic constituents | | | | | | | in volume % | | | | 3.3 | agglomeration of particles, many of which record individual, diverse histories | | | |
 | elemental carbon | | usually plagioclase tectosilicate | in volume % | | in volume % | | | | millimeters | | | | June 25, 1983 7:00 pm | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | | oldest and most primitive rock in solar system | | | | | | | | 1691 | | | in weight % | | | | | | | | | | | | 4.61 kg | rare relative to other chondrite types | less than 950 degree Celsius during its entire history since solidification | | | | Ningqiang | | Ningqiang County, Shaanxi Province, China | meteorite fall | | | | | | | | | in weight % | | definition goes here | Zijin Shan Observatory, Academia Sinica, in Nanjing, Jiangsu Province, China | | often minerals not found on Earth | definition goes here | | | | 32° 55.5' N., 105° 54.4' E. | | 485755 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | 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 |
Novo Urei | | | | | sub-grain boundaries may be prominent | | | | | from 20 GPa to 100 GPa | | | | greater extent of fracturing, undulatory extinction, and kink banding | AURE | may be cloudy due to glassy inclusions | | | partial melting residue | Fo% 79 | Wo% 10 En% 72 | | no chondrules | | | | | | | | | | coarse-grained granular | curved meeting in triple junctions | shock metamorphism | recorded by eyewitness or instruments | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | | | | | | | | | | 1691 | | | | | 0 % | | | | | | olivine-pigeonite about 90% by volume | medium | | | | | | | | diamonds and/or lonsdaleite | 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 | meteorite fall | Berkley et. al (1980) | 0.31 in modal pyroxene/(pryroxene+olivine) | | | | | S4-S6 | | | | | | 1 mm | often minerals not found on Earth | | carbon, metal, sulfides small silicate grains along grain boundaries less than 10% by volume | | olivine, pyroxene (some combination of pigeonite, orthopyroxene, augite) | in degrees, minutes and seconds of lattitude and longitude | | 485755 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | | | | | large, anhedral olivine and pyroxene grains | reduced rims contacting carbonaceous matrix material 0.1 mm FeO-free olivine and/or enstatite rims riddled with tiny inclusions of low-Ni metal | |
Orgueil | in weight % | 3 to 5 % by weight | | | | all fine-grained, opaque | Ivuna meteorite | | | | | strong | greater than 99 % by volume | | | | | agglomeration of particles, many of which record individual, diverse histories | | | |
 | elemental carbon | providing insight into geological evolution of parent asteroid | usually plagioclase tectosilicate | 0 % by volume | | less than 1 % by volume | 8 % of meteorite falls | | | no chondrules | | | aqueous altermation | May 14, 1864 few minutes after 8:00 pm | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | | oldest and most primitive rock in solar system | | | | | | | | 36 | high | 1 | 18 to 22 % by weight | | | | | | | | | | | | 11 kg | rare relative to other chondrite types | less than 950 degree Celsius during its entire history since solidification | | | | Orgueil | | strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocity | CI chondrite | | | | friable | | | | | in weight % | | definition goes here | | | often minerals not found on Earth | definition goes here | | | | 43° 53' N., 1° 23' E. | | 2577 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | less than 1 % by volume | asteroid smaller than 100 km in diameter | no chondrules | | | | which depends on degree of aqueous alteration and thermal metamorphism |
Parnallee | in weight % | 0.2 to 1 % by weight | amphoterite | | | clastic and minor opaque | | | | | | none | 10 to 15 % by volume | | | | 3.6 | agglomeration of particles, many of which record individual, diverse histories | | | |
 | | | minor primary grains only | 2 % by volume | | 0.1 to 1 % by volume | | | | 0.9 millimeters | | | | February 1857 | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | clear, isotropic, variable abundance | 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 | 5 | | 3 | 0.3 to 3 % by weight | | | | | 20 % of total iron | none | | | | | | 77.6 kg | most common chondrite observed from falls | less than 950 degree Celsius during its entire history since solidification | | | | Parnallee | | Perunali, Ramnad district, 52 miles SSE of Madura | meteorite fall | | | | | | | | | in weight % | | definition goes here | | | often minerals not found on Earth | predominantly monoclinic | | | | 9° 14' N., 78° 21' E. | greater than 5 % deviations | 90 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | 60 to 80 % by volume | asteroid smaller than 100 km in diameter | chondrules very sharply defined | about 2 % | | | which depends on degree of aqueous alteration and thermal metamorphism |
Peekskill | in weight % | less than 0.2 % by weight | bronzite chondrite | the range over at which the alteration took place | | transparent, recrystallized, coarse 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, grains greater than 50 microns | 10 % by volume | | 0.1 to 1 % by volume | | | | 0.3 millimeters | | | thermal metamorphism | 7:48 pm October 9, 1992 | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | 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 | 44 | | 6 | less than 1.5 % by weight | only recovered piece collided with a car | | | | 75 % of total iron | strong | | | | | | 12.4 kg | most common chondrite observed from falls | less than 950 degree Celsius during its entire history since solidification | | | | Peekskill | | 207 Wells St. | meteorite fall | | | | | | | | | in weight % | | definition goes here | | | often minerals not found on Earth | orthorhombic | | | | 41° 17' N., 73° 55' W. | homogeneous | 11357 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | 60 to 80 % by volume | asteroid smaller than 100 km in diameter | chondrules poorly defined | 12 to 21 % | | | which depends on degree of aqueous alteration and thermal metamorphism |
Peņa Blanca Spring | | | | | | | | | | | | | | | AUB | | | | melted and crystallized residues from partial melting | | |
 | no chondrules | | | | | | | | | | breccias of igneous lithologies | | | 1:15 pm August 2, 1946 | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | | | | | highly reduced with very little FeO | | | | | 9 | | | | | | | | | | | enstatite | | | | 70 kg | | | | | | Peņa Blanca | | small pond on the Gage Ranch nine miles southeast of Marathon, Texas | meteorite fall | | | | | | | | | | | | | | often minerals not found on Earth | | | | enstatite, forsterite, sodic plagioclase, metal, numerous sulfides | 30° 7.5' N., 103° 7' W. | | 1205 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | | | | | | | |
Pillistfer | in weight % | less than 0.2 % by weight | E chondrite | the range over at which the alteration took place | undulatory extinction, irregular fractures | transparent, recrystallized, coarse crystals | | the nature and degree of thermal metamorphism or aqueous alteration | | 5 to 10 GPa | | | less than 2 to 15 % by volume | | | | | agglomeration of particles, many of which record individual, diverse histories | | | |
 | | providing insight into geological evolution of parent asteroid | secondary, grains greater than 50 microns | 15 % by volume | | 0.1 to 1 % by volume | | | zero | 0.6 millimeters | | | shock metamorphism | 12:30 pm August 8, 1868 | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | 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 | highly reduced with very little FeO | | | | low | 1691 | | 3 to 6 | less than 1.5 % by weight | | | undulatory extinction, irregular fractures, some planar fractures | undulatory extinction, irregular fractures | | strong | | | very weakly shocked | | | 23.25 kg | | less than 950 degree Celsius during its entire history since solidification | | | orthopyroxene for enstatite chondrite | Pillistfer | before, during or after other types of metamorphism | Aukoma, Kurla, Wahhe, and Sawiauk in Estonian SSR | S2 shock stage chondrite | | | | | | | S2 | | in weight % | | definition goes here | | | often minerals not found on Earth | orthorhombic | | | | 58° 40' N., 25° 44' E. | homogeneous | 485755 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | 60 to 80 % by volume | asteroid smaller than 100 km in diameter | chondrules poorly defined | | | | which depends on degree of aqueous alteration and thermal metamorphism |
Portales Valley | in weight % | less than 0.2 % by weight | bronzite chondrite | the range over at which the alteration took place | sharp optical extinction, irregular fractures | transparent, recrystallized, coarse crystals | | the nature and degree of thermal metamorphism or aqueous alteration | | less than 5 GPa | | | 10 to 15 % by volume | | | | | agglomeration of particles, many of which record individual, diverse histories | | | |
 | | providing insight into geological evolution of parent asteroid | secondary, grains greater than 50 microns | 10 % by volume | | 0.1 to 1 % by volume | | | | 0.3 millimeters | | | shock metamorphism | 7:32 am June 13, 1998 | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | 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 | 44 | | 6 | less than 1.5 % by weight | | | sharp optical extinction, irregular fractures | sharp optical extinction, irregular fractures | 75 % of total iron | strong | | | unshocked | | | 80 kg | most common chondrite observed from falls | less than 950 degree Celsius during its entire history since solidification | | | orthopyroxene for enstatite chondrite | Portales Valley | before, during or after other types of metamorphism | eastern New Mexico | S1 shock stage chondrite | | | | | | | S1 | | in weight % | | definition goes here | | | often minerals not found on Earth | orthorhombic | | | | 34° 10.5' N., 103° 17.7' W. | homogeneous | 11357 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | 60 to 80 % by volume | asteroid smaller than 100 km in diameter | chondrules poorly defined | 12 to 21 % | | | which depends on degree of aqueous alteration and thermal metamorphism |
Renazzo | in weight % | 0.8 to 2.6 % by weight | | | undulatory extinction, irregular fractures | mostly fine, opaque | ??? meteorite | the nature and degree of thermal metamorphism or aqueous alteration | | 5 to 10 GPa | | moderate | 30 to 50 % by volume | | | | | agglomeration of particles, many of which record individual, diverse histories | | | |
 | elemental carbon | providing insight into geological evolution of parent asteroid | minor primary grains only | 5 to 8 % by volume | | 0.5 % by volume | | | | 0.7 millimeters | | | shock metamorphism | January 15, 1824 8:30 pm | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | preserved | oldest and most primitive rock in solar system | greater than 0.5 % by weight | less than 20 % by weight; taenite minor or absent | | | | | | 1691 | | 2 | 2 to 16 % by weight | | | undulatory extinction, irregular fractures, some planar fractures | undulatory extinction, irregular fractures | | | | | very weakly shocked | | | 10 kg | rare relative to other chondrite types | less than 950 degree Celsius during its entire history since solidification | | | orthopyroxene for enstatite chondrite | Renazzo | before, during or after other types of metamorphism | Renazzo, Italy | S2 shock stage chondrite | | | | | | | S2 | | in weight % | | definition goes here | | | often minerals not found on Earth | predominantly monoclinic | | | | 44° 46' N., 11° 17' E. | greater than 5 % deviations | 485755 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | 50 to 60 % by volume | asteroid smaller than 100 km in diameter | chondrules very sharply defined | | | | which depends on degree of aqueous alteration and thermal metamorphism |
Soko Banja | in weight % | less than 0.2 % by weight | amphoterite | the range over at which the alteration took place | | transparent, recrystallized, small 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, grains than 2 microns | 2 % by volume | | 0.1 to 1 % by volume | | | | 0.9 millimeters | | | thermal metamorphism | October 13, 1877 | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | 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 | | | | | low | 2 | | 4 | less than 1.5 % by weight | | | | | 20 % of total iron | weak | | | | | | 80 kg | most common chondrite observed from falls | less than 950 degree Celsius during its entire history since solidification | | | | Soko Banja | | Serbia, Yugoslavia | meteorite fall | | | | | | | | | in weight % | | definition goes here | | | often minerals not found on Earth | greater than 20 % monoclinic | | | | 43° 40' N., 21° 52' E. | less than 5 % mean deviations | 124 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | 60 to 80 % by volume | asteroid smaller than 100 km in diameter | chondrules well defined | about 2 % | | | which depends on degree of aqueous alteration and thermal metamorphism |
Tatahouine | | | | | | | | | | | | | | | ADIO | | | | cumulates, crystallized melts, impact mixing | | |
 | no chondrules | | | | | | | | | | coarse-grained orthopyroxenites, gabbros, fine- to coarse-grained basalts, brecciated | | | 1:30 am June 27, 1931 | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | | | | | | | | | | 8 | | | | | | | | | | | hyperstene | | | | 13.5 kg | | | formed by separation of molten rock in a gravity field | | | Tatahouine | | Foum Tatahouine, 4 km NE of a small village in Tunisia | meteorite fall | | | | | | | | | | Howardite, Eucrite, Diogenite | | | | often minerals not found on Earth | | | | orthopyroxene, olivine, chromite; pigeonite, calcic plagioclase, silica | 32° 57' N., 10° 25' E. | | 68 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | | | | | | | |
Tieschitz | in weight % | 0.2 to 1 % by weight | hypersthene chondrite | | | clastic and minor opaque | | | | | | none | 10 to 15 % by volume | | | | 3.6 | agglomeration of particles, many of which record individual, diverse histories | | | |
 | | | minor primary grains only | 5 % by volume | | 0.1 to 1 % by volume | | | | 0.7 millimeters | | | | 1:45 pm July 15, 1878 | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | clear, isotropic, variable abundance | 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 | 10 | | 3 | 0.3 to 3 % by weight | | | | | 50 % of total iron | none | | | | | | 27.4 kg | most common chondrite observed from falls | less than 950 degree Celsius during its entire history since solidification | | | | Tieschitz | | Prostejov, Jihomoravsky, Czechoslovakia | meteorite fall | | | | | | | | | in weight % | | definition goes here | | | often minerals not found on Earth | predominantly monoclinic | | | | 49° 36' N., 17° 7' E. | greater than 5 % deviations | 131 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | 60 to 80 % by volume | asteroid smaller than 100 km in diameter | chondrules very sharply defined | 5 to 10 % | | | which depends on degree of aqueous alteration and thermal metamorphism |
Vigarano | in weight % | 0.2 to 1 % by weight | CV3R chondrite | | undulatory extinction, irregular fractures | clastic and minor opaque | Vigarano meteorite | the nature and degree of thermal metamorphism or aqueous alteration | | 5 to 10 GPa | | weak | 40 % by volume | | | | 3.3 | agglomeration of particles, many of which record individual, diverse histories | | | |
 | elemental carbon | providing insight into geological evolution of parent asteroid | minor primary grains only | 0 to 5 % by volume | | 10 % by volume | | | | 1.0 millimeters | | | shock metamorphism | January 22, 1910 9:30 pm | which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site | | | clear, isotropic, variable abundance | 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 | | | | | | 1691 | | 3 | 0.3 to 3 % by weight | | | undulatory extinction, irregular fractures, some planar fractures | undulatory extinction, irregular fractures | | none | | | very weakly shocked | | | 16 kg | rare relative to other chondrite types | less than 950 degree Celsius during its entire history since solidification | | | orthopyroxene for enstatite chondrite | Vigarano | before, during or after other types of metamorphism | Emilia, Italy | S2 shock stage chondrite | | | | | | | S2 | | in weight % | | definition goes here | | | often minerals not found on Earth | predominantly monoclinic | | | | 44° 51' N., 11° 24' E. | greater than 5 % deviations | 485755 kg | which appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity | 45 % by volume | asteroid smaller than 100 km in diameter | chondrules very sharply defined | | | | which depends on degree of aqueous alteration and thermal metamorphism |