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meteorite fall comparison table
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
Abeein weight %less than 0.2 % by weightE chondritethe 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 asteroidsecondary, grains than 2 microns8 % by volume 0.1 to 1 % by volume  zero0.2 millimeters  thermal metamorphism11:05 pm June 9, 1952which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site  devitrified, absentoldest and most primitive rock in solar systemless than 0.5 % by weightgreater than 20 % by weight, kamacite and taenite in exsolution relationshiphighly reduced with very little FeO   high1691 3 to 5less than 1.5 % by weightmelt breccia    weak     107 kg less than 950 degree Celsius during its entire history since solidification   Abee Abee, Albertameteorite fall        in weight % definition goes here  often minerals not found on Earthgreater than 20 % monoclinic   54° 13' N., 113° 0' W.less than 5 % mean deviations485755 kgwhich appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity60 to 80 % by volumeasteroid smaller than 100 km in diameterchondrules well defined   which depends on degree of aqueous alteration and thermal metamorphism
Allendein weight %0.2 to 1 % by weightCV3OxA chondrite  clastic and minor opaqueAllende meteorite    weak40 % by volume   3.2agglomeration of particles, many of which record individual, diverse histories   
elemental carbon minor primary grains only0 to 5 % by volume 10 % by volume   1.0 millimeters   February 8, 1969 1:05 amseveral tonsiron rich olivine matrix, 24 % iron, rare flecks of iron-nickel clear, isotropic, variable abundanceoldest and most primitive rock in solar systemless than 0.5 % by weightgreater than 20 % by weight, kamacite and taenite in exsolution relationship     1691 30.3 to 3 % by weight     none      rare relative to other chondrite typesless than 950 degree Celsius during its entire history since solidification   Allende village of Pueblito de Allende, Chihuahua State, Mexicometeorite fall        in weight % definition goes here  often minerals not found on Earthpredominantly monoclinic   26° 58' N., 105° 19' W.greater than 5 % deviations485755 kg
45 % by volumeasteroid smaller than 100 km in diameterchondrules 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, 1869which 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, Brazilmeteorite fall             often minerals not found on Earth   Al-Ti-diopside, anorthite, calcic olivine22° 58' S., 44° 19' W. 485755 kgwhich 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, 1999which 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 meteoroidshyperstene   25 kg  formed by separation of molten rock in a gravity field  Bilanga Bilanga Yanga and Gomponsago, Burkina Faso, Africaoriented meteorite       conical from preferential ablation during atmospheric passage Howardite, Eucrite, Diogenite   often minerals not found on Earth   orthopyroxene, olivine, chromite; pigeonite, calcic plagioclase, silica12° 27' N., 0° 05' W. 68 kgwhich appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity       
Bruderheimin weight %less than 0.2 % by weighthypersthene chondritethe 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 asteroidsecondary, grains greater than 50 microns5 % by volume 0.1 to 1 % by volume   0.7 millimeters  thermal metamorphismMarch 4, 1960which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site  devitrified, absentoldest and most primitive rock in solar systemless than 0.5 % by weightgreater than 20 % by weight, kamacite and taenite in exsolution relationship    low155 6less than 1.5 % by weight    50 % of total ironstrong     400 kgmost common chondrite observed from fallsless than 950 degree Celsius during its entire history since solidification   Bruderheim Alberta, Canadameteorite fall        in weight % definition goes here  often minerals not found on Earthorthorhombic   53° 54' N., 112° 53' W.homogeneous4673 kg
60 to 80 % by volumeasteroid smaller than 100 km in diameterchondrules poorly defined5 to 10 %  which depends on degree of aqueous alteration and thermal metamorphism
Dyalpur    completely shattered or mosaicized    100 GPa or greater    AUREmottled by melt glass  partial melting residueFo% 84Wo% 11 En% 76 no chondrules         coarse-grained granular shock metamorphismrecorded by eyewitness or instrumentswhich 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 volumeshock melted       diamonds and/or lonsdaleitebased on the locale, region, or nearby town in which the fall occurred strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocitymeteorite fallBerkley et. al (1980)0.41 in modal pyroxene/(pryroxene+olivine)    shock melted     much less than 1 mmoften 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 kgwhich appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity    mosaicizedreduced rims contacting carbonaceous matrix material 0.1 mm FeO-free olivine and/or enstatite rims riddled with tiny inclusions of low-Ni metal 
Grosnajain weight %0.2 to 1 % by weightCV3OxB chondrite planar fractures, undulatory extinction, irregular fracturesclastic and minor opaqueBali meteoritethe nature and degree of thermal metamorphism or aqueous alteration 15 to 20 GPa weak40 % by volume   3.3agglomeration of particles, many of which record individual, diverse histories   
elemental carbonproviding insight into geological evolution of parent asteroidminor primary grains only0 to 5 % by volume 10 % by volume   1.0 millimeters  shock metamorphismJune 28, 1861 7:00 pmwhich can over an order of magnitude greater than total mass of fragment(s) collected at the impact site  clear, isotropic, variable abundanceoldest and most primitive rock in solar systemless than 0.5 % by weightgreater than 20 % by weight, kamacite and taenite in exsolution relationship     1691 30.3 to 3 % by weight  clinoenstatite lamellae on (100), undulatory extinction, planar fractures, irregular fracturesundulatory extinction none  weakly shocked  3.5 kgrare relative to other chondrite typesless than 950 degree Celsius during its entire history since solidification  orthopyroxene for enstatite chondriteGrosnajabefore, during or after other types of metamorphismstrewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocityS3 shock stage chondrite      S3 in weight % definition goes here  often minerals not found on Earthpredominantly monoclinic   43° 40' N., 45° 23' E.greater than 5 % deviations485755 kgwhich appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity45 % by volumeasteroid smaller than 100 km in diameterchondrules very sharply defined   which depends on degree of aqueous alteration and thermal metamorphism
Havero    completely shattered or mosaicized    100 GPa or greater    AUREmottled by melt glass  partial melting residueFo% 79Wo% 2.5 En% 81 clinobronzite no chondrules         coarse-grained granularcurved meeting in triple junctionsshock metamorphismrecorded by eyewitness or instrumentswhich 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 volumeshock melted       diamonds and/or lonsdaleitebased on the locale, region, or nearby town in which the fall occurred strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocitymeteorite fallBerkley et. al (1980)0.17 in modal pyroxene/(pryroxene+olivine)    shock melted     much less than 1 mmoften 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 kgwhich appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity    mosaicizedreduced rims contacting carbonaceous matrix material 0.1 mm FeO-free olivine and/or enstatite rims riddled with tiny inclusions of low-Ni metal 
Holbrookin weight %less than 0.2 % by weighthypersthene chondritethe 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 asteroidsecondary, grains greater than 50 microns5 % by volume 0.1 to 1 % by volume   0.7 millimeters  thermal metamorphism7:15 pm July 19, 1912which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site  devitrified, absentoldest and most primitive rock in solar systemless than 0.5 % by weightgreater than 20 % by weight, kamacite and taenite in exsolution relationship    low155 6less than 1.5 % by weight    50 % of total ironstrong     217.9 kgmost common chondrite observed from fallsless than 950 degree Celsius during its entire history since solidification   Holbrook Navajo County, Arizonameteorite fall        in weight % definition goes here  often minerals not found on Earthorthorhombic   34° 54' N., 110° 11' W.homogeneous4673 kgwhich appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity60 to 80 % by volumeasteroid smaller than 100 km in diameterchondrules poorly defined5 to 10 %  which depends on degree of aqueous alteration and thermal metamorphism
Indarchin weight %less than 0.2 % by weightE chondritethe range over at which the alteration took placeplanar fractures, undulatory extinction, irregular fracturestransparent, 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 asteroidsecondary, grains than 2 microns8 % by volume 0.1 to 1 % by volume  zero0.2 millimeters  shock metamorphism8:10 pm April 7, 1891which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site  devitrified, absentoldest and most primitive rock in solar systemless than 0.5 % by weightgreater than 20 % by weight, kamacite and taenite in exsolution relationshiphighly reduced with very little FeO   high1691 3 to 5less than 1.5 % by weight  clinoenstatite lamellae on (100), undulatory extinction, planar fractures, irregular fracturesundulatory extinction weak  weakly shocked  27 kg less than 950 degree Celsius during its entire history since solidification  orthopyroxene for enstatite chondriteIndarchbefore, during or after other types of metamorphismAzerbaydzhan SSR, USSRS3 shock stage chondrite      S3 in weight % definition goes here  often minerals not found on Earthgreater than 20 % monoclinic   39° 45' N., 46° 40' E.less than 5 % mean deviations485755 kgwhich appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity60 to 80 % by volumeasteroid smaller than 100 km in diameterchondrules 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, 1924which 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, Coloradometeorite fall         Howardite, Eucrite, Diogenite   often minerals not found on Earth   orthopyroxene, olivine, chromite; pigeonite, calcic plagioclase, silica40° 21' N., 104° 54' W. 68 kgwhich appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity       
Kakangariin weight %0.2 to 1 % by weight   clastic and minor opaqueKakangari meteorite    none73 % by volume (including metal)   3.6agglomeration of particles, many of which record individual, diverse histories   
  minor primary grains only0 % by volume (included in matrix abundance) less than 0.1 % by volume   0.6 millimeters   June 4, 1890which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site  clear, isotropic, variable abundanceoldest and most primitive rock in solar systemless than 0.5 % by weightgreater than 20 % by weight, kamacite and taenite in exsolution relationship     1691 30.3 to 3 % by weight     none       less than 950 degree Celsius during its entire history since solidification   Kakangari Kangankarai, Indiameteorite fall        in weight % definition goes here  often minerals not found on Earthpredominantly monoclinic   12° 23' N., 78° 31' E.greater than 5 % deviations485755 kgwhich appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity27 % by volumeasteroid smaller than 100 km in diameterchondrules 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, 1942which 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, Sudanmeteorite fall         Howardite, Eucrite, Diogenite   often minerals not found on Earth   orthopyroxene, olivine, chromite; pigeonite, calcic plagioclase, silica31° 10' S., 127° 45' E. 41 kgwhich 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 bandingAUREmay be cloudy due to glassy inclusions  partial melting residueFo% 79Wo% 7.7 En% 74 no chondrules         coarse-grained granularcurved meeting in triple junctionsshock metamorphismrecorded by eyewitness or instrumentswhich 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 volumemedium       diamonds and/or lonsdaleitebased on the locale, region, or nearby town in which the fall occurred strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocitymeteorite fallMalhotra (1962), Bhandari et al. (1981)     S4-S6     1 mmoften 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 kgwhich appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity    large, anhedral olivine and pyroxene grainsreduced 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 historiesultrametamorphism, partial melting with some melt migration  
no chondrules         fine- to coarse-grained equigranular  2:00 pm October 1, 1868which 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, Pakistanmeteorite fall             iron, pyroxene, olivine subcondritic abundances of plagioclase and troilite;   olivine, orthopyroxene, clinopyroxene, metal with some troilite and some sodic plagioclase29° 32' N., 71° 48' E. 485755 kgwhich 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, 1902which 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 centimeter0.3 to 2.8 % by volume45 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 yearsfrom 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 kgwhich 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, 1974which 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 Nigeriameteorite fall             often minerals not found on Earth   enstatite, forsterite, sodic plagioclase, metal, numerous sulfides8° 58' N., 12° 5' E. 1205 kgwhich appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity       
Monahans (1998)in weight %less than 0.2 % by weightbronzite chondritethe range over at which the alteration took placeweak mosaicism, planar fracturestransparent, 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 asteroidsecondary, 2 to 50 micron grains10 % by volume 0.1 to 1 % by volume   0.3 millimeters  shock metamorphism6:47 pm March 22, 1998which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site  devitrified, absentoldest and most primitive rock in solar systemless than 0.5 % by weightgreater than 20 % by weight, kamacite and taenite in exsolution relationship    high76 5less than 1.5 % by weight  weak mosaicism, twinning on (100), planar fracturesundulatory extinction, partially isotropic, planar deformation features75 % of total ironmoderate  moderately shocked  2.587 kgmost common chondrite observed from fallsless than 950 degree Celsius during its entire history since solidification  orthopyroxene for enstatite chondriteMonahans (1998)before, during or after other types of metamorphismAllen Street, Monahans, TexasS4 shock stage chondrite      S4 in weight % definition goes here  often minerals not found on Earthless than 20 % monoclinic   102° 53.5' W., 31° 36.5' N.homogeneous1267 kgwhich appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity60 to 80 % by volumeasteroid smaller than 100 km in diameterchondrules readily delineated12 to 21 %  which depends on degree of aqueous alteration and thermal metamorphism
Mount Tazerzaitin weight %less than 0.2 % by weighthypersthene chondritethe range over at which the alteration took placesharp optical extinction, irregular fracturestransparent, 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 asteroidsecondary, 2 to 50 micron grains5 % by volume 0.1 to 1 % by volume   0.7 millimeters  shock metamorphismAugust 21, 1991which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site  devitrified, absentoldest and most primitive rock in solar systemless than 0.5 % by weightgreater than 20 % by weight, kamacite and taenite in exsolution relationship    low44 5less than 1.5 % by weight  sharp optical extinction, irregular fracturessharp optical extinction, irregular fractures50 % of total ironmoderate  unshocked  110 kgmost common chondrite observed from fallsless than 950 degree Celsius during its entire history since solidification  orthopyroxene for enstatite chondriteMt. Tazerzaitbefore, during or after other types of metamorphismTahoua, Republic of NigerS1 shock stage chondrite      S1 in weight % definition goes here  often minerals not found on Earthless than 20 % monoclinic   18° 42' N., 4° 48' E.homogeneous1256 kgwhich appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity60 to 80 % by volumeasteroid smaller than 100 km in diameterchondrules readily delineated5 to 10 %  which depends on degree of aqueous alteration and thermal metamorphism
Murchisonin weight %0.8 to 2.6 % by weight  sharp optical extinction, irregular fracturesmostly fine, opaqueMighei meteoritethe nature and degree of thermal metamorphism or aqueous alteration less than 5 GPa moderate70 % by volume    agglomeration of particles, many of which record individual, diverse histories   
elemental carbonproviding insight into geological evolution of parent asteroidminor primary grains only0.1 % by volume 5 % by volume   0.3 millimeters  shock metamorphismSeptember 28, 1969 10:45 amwhich can over an order of magnitude greater than total mass of fragment(s) collected at the impact sitecontain amino acids rareoldest and most primitive rock in solar systemgreater than 0.5 % by weightless than 20 % by weight; taenite minor or absent     1691 22 to 16 % by weight  sharp optical extinction, irregular fracturessharp optical extinction, irregular fractures    unshocked   rare relative to other chondrite typesless than 950 degree Celsius during its entire history since solidification  orthopyroxene for enstatite chondriteMurchisonbefore, during or after other types of metamorphismMurchison, Victoria, AustraliaS1 shock stage chondrite   friable  S1 in weight % definition goes here  often minerals not found on Earthpredominantly monoclinic   36° 37' S., 145° 12' E.greater than 5 % deviations485755 kgwhich appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity20 % by volumeasteroid smaller than 100 km in diameterchondrules very sharply defined   which depends on degree of aqueous alteration and thermal metamorphism
Ningqiangin weight %in weight %   fine grained disequilibrium mixture of silicates, oxides, metal, sulfides and organic constituents      in volume %   3.3agglomeration of particles, many of which record individual, diverse histories   
elemental carbon usually plagioclase tectosilicatein volume % in volume %   millimeters   June 25, 1983 7:00 pmwhich 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 kgrare relative to other chondrite typesless than 950 degree Celsius during its entire history since solidification   Ningqiang Ningqiang County, Shaanxi Province, Chinameteorite fall        in weight % definition goes hereZijin Shan Observatory, Academia Sinica, in Nanjing, Jiangsu Province, China often minerals not found on Earthdefinition goes here   32° 55.5' N., 105° 54.4' E. 485755 kgwhich appears as an elongated footprint which depends on impact angle, airbursts, and impact velocityin volume %asteroid smaller than 100 km in diametersmall 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 bandingAUREmay be cloudy due to glassy inclusions  partial melting residueFo% 79Wo% 10 En% 72 no chondrules         coarse-grained granularcurved meeting in triple junctionsshock metamorphismrecorded by eyewitness or instrumentswhich 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 volumemedium       diamonds and/or lonsdaleitebased on the locale, region, or nearby town in which the fall occurred strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocitymeteorite fallBerkley et. al (1980)0.31 in modal pyroxene/(pryroxene+olivine)    S4-S6     1 mmoften 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 kgwhich appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity    large, anhedral olivine and pyroxene grainsreduced rims contacting carbonaceous matrix material 0.1 mm FeO-free olivine and/or enstatite rims riddled with tiny inclusions of low-Ni metal 
Orgueilin weight %3 to 5 % by weight   all fine-grained, opaqueIvuna meteorite    stronggreater than 99 % by volume    agglomeration of particles, many of which record individual, diverse histories   
elemental carbonproviding insight into geological evolution of parent asteroidusually plagioclase tectosilicate0 % by volume less than 1 % by volume8 % of meteorite falls  no chondrules  aqueous altermationMay 14, 1864 few minutes after 8:00 pmwhich 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       36high118 to 22 % by weight           11 kgrare relative to other chondrite typesless than 950 degree Celsius during its entire history since solidification   Orgueil strewn fields, elongated footprints which depends on impact angle, airbursts, and impact velocityCI chondrite   friable    in weight % definition goes here  often minerals not found on Earthdefinition goes here   43° 53' N., 1° 23' E. 2577 kgwhich appears as an elongated footprint which depends on impact angle, airbursts, and impact velocityless than 1 % by volumeasteroid smaller than 100 km in diameterno chondrules   which depends on degree of aqueous alteration and thermal metamorphism
Parnalleein weight %0.2 to 1 % by weightamphoterite  clastic and minor opaque     none10 to 15 % by volume   3.6agglomeration of particles, many of which record individual, diverse histories   
  minor primary grains only2 % by volume 0.1 to 1 % by volume   0.9 millimeters   February 1857which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site  clear, isotropic, variable abundanceoldest and most primitive rock in solar systemless than 0.5 % by weightgreater than 20 % by weight, kamacite and taenite in exsolution relationship    low5 30.3 to 3 % by weight    20 % of total ironnone     77.6 kgmost common chondrite observed from fallsless than 950 degree Celsius during its entire history since solidification   Parnallee Perunali, Ramnad district, 52 miles SSE of Madurameteorite fall        in weight % definition goes here  often minerals not found on Earthpredominantly monoclinic   9° 14' N., 78° 21' E.greater than 5 % deviations90 kgwhich appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity60 to 80 % by volumeasteroid smaller than 100 km in diameterchondrules very sharply definedabout 2 %  which depends on degree of aqueous alteration and thermal metamorphism
Peekskillin weight %less than 0.2 % by weightbronzite chondritethe 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 asteroidsecondary, grains greater than 50 microns10 % by volume 0.1 to 1 % by volume   0.3 millimeters  thermal metamorphism7:48 pm October 9, 1992which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site  devitrified, absentoldest and most primitive rock in solar systemless than 0.5 % by weightgreater than 20 % by weight, kamacite and taenite in exsolution relationship    high44 6less than 1.5 % by weightonly recovered piece collided with a car   75 % of total ironstrong     12.4 kgmost common chondrite observed from fallsless 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 Earthorthorhombic   41° 17' N., 73° 55' W.homogeneous11357 kgwhich appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity60 to 80 % by volumeasteroid smaller than 100 km in diameterchondrules poorly defined12 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, 1946which 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, Texasmeteorite fall             often minerals not found on Earth   enstatite, forsterite, sodic plagioclase, metal, numerous sulfides30° 7.5' N., 103° 7' W. 1205 kgwhich appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity       
Pillistferin weight %less than 0.2 % by weightE chondritethe range over at which the alteration took placeundulatory extinction, irregular fracturestransparent, 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 asteroidsecondary, grains greater than 50 microns15 % by volume 0.1 to 1 % by volume  zero0.6 millimeters  shock metamorphism12:30 pm August 8, 1868which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site  devitrified, absentoldest and most primitive rock in solar systemless than 0.5 % by weightgreater than 20 % by weight, kamacite and taenite in exsolution relationshiphighly reduced with very little FeO   low1691 3 to 6less than 1.5 % by weight  undulatory extinction, irregular fractures, some planar fracturesundulatory extinction, irregular fractures strong  very weakly shocked  23.25 kg less than 950 degree Celsius during its entire history since solidification  orthopyroxene for enstatite chondritePillistferbefore, during or after other types of metamorphismAukoma, Kurla, Wahhe, and Sawiauk in Estonian SSRS2 shock stage chondrite      S2 in weight % definition goes here  often minerals not found on Earthorthorhombic   58° 40' N., 25° 44' E.homogeneous485755 kgwhich appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity60 to 80 % by volumeasteroid smaller than 100 km in diameterchondrules poorly defined   which depends on degree of aqueous alteration and thermal metamorphism
Portales Valleyin weight %less than 0.2 % by weightbronzite chondritethe range over at which the alteration took placesharp optical extinction, irregular fracturestransparent, 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 asteroidsecondary, grains greater than 50 microns10 % by volume 0.1 to 1 % by volume   0.3 millimeters  shock metamorphism7:32 am June 13, 1998which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site  devitrified, absentoldest and most primitive rock in solar systemless than 0.5 % by weightgreater than 20 % by weight, kamacite and taenite in exsolution relationship    high44 6less than 1.5 % by weight  sharp optical extinction, irregular fracturessharp optical extinction, irregular fractures75 % of total ironstrong  unshocked  80 kgmost common chondrite observed from fallsless than 950 degree Celsius during its entire history since solidification  orthopyroxene for enstatite chondritePortales Valleybefore, during or after other types of metamorphismeastern New MexicoS1 shock stage chondrite      S1 in weight % definition goes here  often minerals not found on Earthorthorhombic   34° 10.5' N., 103° 17.7' W.homogeneous11357 kgwhich appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity60 to 80 % by volumeasteroid smaller than 100 km in diameterchondrules poorly defined12 to 21 %  which depends on degree of aqueous alteration and thermal metamorphism
Renazzoin weight %0.8 to 2.6 % by weight  undulatory extinction, irregular fracturesmostly fine, opaque??? meteoritethe nature and degree of thermal metamorphism or aqueous alteration 5 to 10 GPa moderate30 to 50 % by volume    agglomeration of particles, many of which record individual, diverse histories   
elemental carbonproviding insight into geological evolution of parent asteroidminor primary grains only5 to 8 % by volume 0.5 % by volume   0.7 millimeters  shock metamorphismJanuary 15, 1824 8:30 pmwhich can over an order of magnitude greater than total mass of fragment(s) collected at the impact site  preservedoldest and most primitive rock in solar systemgreater than 0.5 % by weightless than 20 % by weight; taenite minor or absent     1691 22 to 16 % by weight  undulatory extinction, irregular fractures, some planar fracturesundulatory extinction, irregular fractures    very weakly shocked  10 kgrare relative to other chondrite typesless than 950 degree Celsius during its entire history since solidification  orthopyroxene for enstatite chondriteRenazzobefore, during or after other types of metamorphismRenazzo, ItalyS2 shock stage chondrite      S2 in weight % definition goes here  often minerals not found on Earthpredominantly monoclinic   44° 46' N., 11° 17' E.greater than 5 % deviations485755 kgwhich appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity50 to 60 % by volumeasteroid smaller than 100 km in diameterchondrules very sharply defined   which depends on degree of aqueous alteration and thermal metamorphism
Soko Banjain weight %less than 0.2 % by weightamphoteritethe 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 asteroidsecondary, grains than 2 microns2 % by volume 0.1 to 1 % by volume   0.9 millimeters  thermal metamorphismOctober 13, 1877which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site  devitrified, absentoldest and most primitive rock in solar systemless than 0.5 % by weightgreater than 20 % by weight, kamacite and taenite in exsolution relationship    low2 4less than 1.5 % by weight    20 % of total ironweak     80 kgmost common chondrite observed from fallsless than 950 degree Celsius during its entire history since solidification   Soko Banja Serbia, Yugoslaviameteorite fall        in weight % definition goes here  often minerals not found on Earthgreater than 20 % monoclinic   43° 40' N., 21° 52' E.less than 5 % mean deviations124 kgwhich appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity60 to 80 % by volumeasteroid smaller than 100 km in diameterchondrules well definedabout 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, 1931which 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 Tunisiameteorite fall         Howardite, Eucrite, Diogenite   often minerals not found on Earth   orthopyroxene, olivine, chromite; pigeonite, calcic plagioclase, silica32° 57' N., 10° 25' E. 68 kgwhich appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity       
Tieschitzin weight %0.2 to 1 % by weighthypersthene chondrite  clastic and minor opaque     none10 to 15 % by volume   3.6agglomeration of particles, many of which record individual, diverse histories   
  minor primary grains only5 % by volume 0.1 to 1 % by volume   0.7 millimeters   1:45 pm July 15, 1878which can over an order of magnitude greater than total mass of fragment(s) collected at the impact site  clear, isotropic, variable abundanceoldest and most primitive rock in solar systemless than 0.5 % by weightgreater than 20 % by weight, kamacite and taenite in exsolution relationship    low10 30.3 to 3 % by weight    50 % of total ironnone     27.4 kgmost common chondrite observed from fallsless than 950 degree Celsius during its entire history since solidification   Tieschitz Prostejov, Jihomoravsky, Czechoslovakiameteorite fall        in weight % definition goes here  often minerals not found on Earthpredominantly monoclinic   49° 36' N., 17° 7' E.greater than 5 % deviations131 kgwhich appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity60 to 80 % by volumeasteroid smaller than 100 km in diameterchondrules very sharply defined5 to 10 %  which depends on degree of aqueous alteration and thermal metamorphism
Vigaranoin weight %0.2 to 1 % by weightCV3R chondrite undulatory extinction, irregular fracturesclastic and minor opaqueVigarano meteoritethe nature and degree of thermal metamorphism or aqueous alteration 5 to 10 GPa weak40 % by volume   3.3agglomeration of particles, many of which record individual, diverse histories   
elemental carbonproviding insight into geological evolution of parent asteroidminor primary grains only0 to 5 % by volume 10 % by volume   1.0 millimeters  shock metamorphismJanuary 22, 1910 9:30 pmwhich can over an order of magnitude greater than total mass of fragment(s) collected at the impact site  clear, isotropic, variable abundanceoldest and most primitive rock in solar systemless than 0.5 % by weightgreater than 20 % by weight, kamacite and taenite in exsolution relationship     1691 30.3 to 3 % by weight  undulatory extinction, irregular fractures, some planar fracturesundulatory extinction, irregular fractures none  very weakly shocked  16 kgrare relative to other chondrite typesless than 950 degree Celsius during its entire history since solidification  orthopyroxene for enstatite chondriteVigaranobefore, during or after other types of metamorphismEmilia, ItalyS2 shock stage chondrite      S2 in weight % definition goes here  often minerals not found on Earthpredominantly monoclinic   44° 51' N., 11° 24' E.greater than 5 % deviations485755 kgwhich appears as an elongated footprint which depends on impact angle, airbursts, and impact velocity45 % by volumeasteroid smaller than 100 km in diameterchondrules very sharply defined   which depends on degree of aqueous alteration and thermal metamorphism

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