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Dong Ujimqin Qi meteorite, East Ujimqin Banner (Dongwuzhumuqin Co.; Dongwu Qi), Xilingol League (Xilinguole Prefecture), Inner Mongolia, Chinai
Regional Level Types
Dong Ujimqin Qi meteoriteMeteorite Fall Location
East Ujimqin Banner (Dongwuzhumuqin Co.; Dongwu Qi)County
Xilingol League (Xilinguole Prefecture)Prefecture
Inner MongoliaAutonomous Region
ChinaCountry

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Latitude & Longitude (WGS84):
45° 30' 0'' North , 119° 1' 59'' East
Latitude & Longitude (decimal):
Mindat Locality ID:
262345
Long-form identifier:
mindat:1:2:262345:3
GUID (UUID V4):
0
Name(s) in local language(s):
, 锡林郭勒盟, 内蒙古自治区, 中国


Mesosiderite (Stony-Iron)
Fall, 7 Sept 1995; 128 kg

On a cloudless day a tremendous sound was heard, black smoke was seen, and 3 meteorite masses with fusion crusts were soon recovered, the largest 88.2 kg. Dong Ujimqin Qi was only the 7th witnessed mesosiderite fall. Mesosiderites normally consist of approximately equal masses of once molten Fe-Ni metal which may have penetrated into a nearly equal mass of now heavily brecciated orthopyroxene-rich silicates. Other silicates (esp. olivine and plagioclase), troilite, chromite, and other minor constituents are found in Dong Ujimqin Qi (as in other mesosiderites). The Ca-poor, slitely variable pyroxene in Dong Ujimqin Qi is usually ~ 24 mol% ferrosilite; plagioclase appears to be mostly anorthite, and the olivine — often found in large crystals several cm in diameter — is unusually Mg-rich. Minor and even trace amounts of such minerals as merrillite, tridymite, and standfieldite is to be expected. The presence of cordierite is a little surprising as it is a metamorphic phase in terrestrial geological environments. Cordierite had, however, been found previously in the Chaunskij mesosiderite.

A number of active and still unresolved hypotheses are under discussion as to how the original mesosiderites were created on an ancient original parent body and/or during a collision between two asteroids. Much later, after presumably being separated from a mother asteroid or asteroidal fragment, Dong Ujimqin Qi experienced a relatively long cosmic exposure age of 250±50 Ma before it eventually collided with the earth.

Over 200 mesosiderites have been found, many of them small, weathered, and fragmented, in the cold and hot desserts of Antarctica, Australia, Africa, the Americas and elsewhere. A good number of them are moderately massive (28 with m> 10 kg by late 2014) and sometimes yield valuable info. However, the brecciated nature of the 'normal' mesosiderite makes them — and especially their sulfides and phosphides — particularly vulnerable to chemical attack in almost any terrestrial environment. Thus, Dong Ujimqin Qi, as the 2nd most massive mesosiderite fall and the 7th most massive mesosiderite overall, is a particularly valuable addition to the mesosiderite collection.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


8 valid minerals.

Meteorite/Rock Types Recorded

Note: data is currently VERY limited. Please bear with us while we work towards adding this information!

Select Rock List Type

Alphabetical List Tree Diagram

Detailed Mineral List:

ⓘ Anorthite
Formula: Ca(Al2Si2O8)
Description: Plagioclase (An91-94) in sections studied by Terribilini et al. (2000)
ⓘ Cordierite
Formula: (Mg,Fe)2Al3(AlSi5O18)
ⓘ 'Fayalite-Forsterite Series'
ⓘ Merrillite
Formula: Ca9NaMg(PO4)7
ⓘ Native Iron
Formula: Fe
ⓘ Native Iron var. Kamacite
Formula: (Fe,Ni)
ⓘ 'Plagioclase'
Formula: (Na,Ca)[(Si,Al)AlSi2]O8
ⓘ 'Pyroxene Group'
Formula: ADSi2O6
Description: Mildly variable pyroxene (Fs22-27) in various regions; However, some zoned pyroxenes with distinctly Fe-poor cores and Fe-rich rims are found in matrix.
ⓘ 'Silica'
Description: Matrix silica is normally found inside plagioclase; Silica also as inclusions in Stanfieldite. One would like to think the silica is tridymite (identified elsewhere in the meteorite), but the microprobe does not reveal crystal structure.
ⓘ Stanfieldite
Formula: Ca4Mg5(PO4)6
ⓘ Taenite
Formula: (Fe,Ni)
ⓘ Tridymite
Formula: SiO2
ⓘ Troilite
Formula: FeS

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
ⓘNative Iron1.AE.05Fe
ⓘvar. Kamacite1.AE.05(Fe,Ni)
ⓘTaenite1.AE.10(Fe,Ni)
Group 2 - Sulphides and Sulfosalts
ⓘTroilite2.CC.10FeS
Group 4 - Oxides and Hydroxides
ⓘTridymite4.DA.10SiO2
Group 8 - Phosphates, Arsenates and Vanadates
ⓘMerrillite8.AC.45Ca9NaMg(PO4)7
ⓘStanfieldite8.AC.70Ca4Mg5(PO4)6
Group 9 - Silicates
ⓘCordierite9.CJ.10(Mg,Fe)2Al3(AlSi5O18)
ⓘAnorthite9.FA.35Ca(Al2Si2O8)
Unclassified
ⓘ'Fayalite-Forsterite Series'-
ⓘ'Plagioclase'-(Na,Ca)[(Si,Al)AlSi2]O8
ⓘ'Pyroxene Group'-ADSi2O6
ⓘ'Silica'-

List of minerals for each chemical element

OOxygen
Oⓘ AnorthiteCa(Al2Si2O8)
Oⓘ Cordierite(Mg,Fe)2Al3(AlSi5O18)
Oⓘ StanfielditeCa4Mg5(PO4)6
Oⓘ TridymiteSiO2
Oⓘ MerrilliteCa9NaMg(PO4)7
Oⓘ Fayalite-Forsterite Series
Oⓘ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Oⓘ Pyroxene GroupADSi2O6
NaSodium
Naⓘ MerrilliteCa9NaMg(PO4)7
Naⓘ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
MgMagnesium
Mgⓘ Cordierite(Mg,Fe)2Al3(AlSi5O18)
Mgⓘ StanfielditeCa4Mg5(PO4)6
Mgⓘ MerrilliteCa9NaMg(PO4)7
Mgⓘ Fayalite-Forsterite Series
AlAluminium
Alⓘ AnorthiteCa(Al2Si2O8)
Alⓘ Cordierite(Mg,Fe)2Al3(AlSi5O18)
Alⓘ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
SiSilicon
Siⓘ AnorthiteCa(Al2Si2O8)
Siⓘ Cordierite(Mg,Fe)2Al3(AlSi5O18)
Siⓘ TridymiteSiO2
Siⓘ Fayalite-Forsterite Series
Siⓘ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Siⓘ Pyroxene GroupADSi2O6
PPhosphorus
Pⓘ StanfielditeCa4Mg5(PO4)6
Pⓘ MerrilliteCa9NaMg(PO4)7
SSulfur
Sⓘ TroiliteFeS
CaCalcium
Caⓘ AnorthiteCa(Al2Si2O8)
Caⓘ StanfielditeCa4Mg5(PO4)6
Caⓘ MerrilliteCa9NaMg(PO4)7
Caⓘ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
FeIron
Feⓘ Cordierite(Mg,Fe)2Al3(AlSi5O18)
Feⓘ Native IronFe
Feⓘ Native Iron var. Kamacite(Fe,Ni)
Feⓘ Taenite(Fe,Ni)
Feⓘ TroiliteFeS
Feⓘ Fayalite-Forsterite Series
NiNickel
Niⓘ Native Iron var. Kamacite(Fe,Ni)
Niⓘ Taenite(Fe,Ni)

Other Regions, Features and Areas containing this locality

Amur PlateTectonic Plate
AsiaContinent
Eurasian Plate

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