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Ilafegh 009 meteorite, Bordj Badji Mokhtar, Bordj Badji Mokhtar District, Bordj Badji Mokhtar Province, Algeriai
Regional Level Types
Ilafegh 009 meteoriteMeteorite Fall Location
Bordj Badji MokhtarCommune
Bordj Badji Mokhtar DistrictDistrict
Bordj Badji Mokhtar ProvinceProvince
AlgeriaCountry

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Latitude & Longitude (WGS84):
21° 37' 59'' North , 1° 16' 0'' East
Latitude & Longitude (decimal):
Köppen climate type:
Mindat Locality ID:
257673
Long-form identifier:
mindat:1:2:257673:5
GUID (UUID V4):
0


Enstatite Chondrite, low iron (EL7; W0/1; S4)
1989 find, 421 g; Shock-melted

Purchased in Algeria, the Ilafegh 009 meteorite is a highly shocked enstatite-rich stone with a composition very similar to that of the EL chondrites. There are, however, no chondrules. More than half of the stone consists of enstatite (mostly orthoenstatite; usually in ~cm-size crystals) with significant quantities of Ni-Fe metal (~27 wt%), troilite (~8 wt%), and plagioclase (~7 wt%). In addition, there are a number of minor phases characteristic of Enstatite Chondrites. Two phases, Ferroan Alabandite and Kamacite with ~1% Si are usually reliable and specific indicators of the EL chemical group. Variable composition in both plagioclase and schreibersite plus various inhomogeneously distributed inclusions indicate rapidly cooling phases unable to reequilibrate after violent heating shocks. Radioactive dating suggests that Ilafegh 009 may have experienced a particularly violent shock event ~4.4 billion years ago — perhaps 150 million years after initial formation of its major components.

Within the meteoritical community, there is serious unease with the proper terminology to use in describing these “shock-melted” meteorites with Enstatite Chondrite-like composition. Part of the problem seems to be that residual heating from original radioactive species and heating from violent events within the Enstatite clan formation zone were coeval and entangled events. McCoy et al. (1995) provide the best overall description of this particular meteorite and also provide a perspective for some of the general issues involved. However, the small amount of available material makes it doubly difficult to stitch together a completely satisfying account of this ancient, complex and intriguing stone.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


10 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:

ⓘ Alabandite
Formula: MnS
Description: Alabandite — Ferroan Alabandite is an indicator for the EL chemical group of Enstatite; Associated with and embedded with troilite
ⓘ Albite
Formula: Na(AlSi3O8)
ⓘ Albite var. Oligoclase
Formula: (Na,Ca)[Al(Si,Al)Si2O8]
ⓘ Clinoenstatite
Formula: MgSiO3
Description: minor, but pervasive
ⓘ Daubréelite
Formula: Fe2+Cr3+2S4
Description: Associated with the more abundant troilite
ⓘ Enstatite
Formula: Mg2Si2O6
Description: Usually as moderately large crystals up to 1 cm in size. Often contains trapped inclusions with diverse mineralogies
ⓘ 'Feldspar Group'
Description: Found in small inclusions within large Enstatite crystals
ⓘ Native Iron
Formula: Fe
Description: abundant, but somewhat disordered in some instances
ⓘ Native Iron var. Kamacite
Formula: (Fe,Ni)
Description: abundant, but somewhat disordered in some instances
ⓘ 'Nickel-iron'
ⓘ Oldhamite
Formula: CaS
ⓘ Osbornite
Formula: TiN
Description: 3 small grains
ⓘ 'Plagioclase'
Formula: (Na,Ca)[(Si,Al)AlSi2]O8
Description: Variable, but with a strong oligoclase component
ⓘ Schreibersite
Formula: (Fe,Ni)3P
Description: Ni-content variable
ⓘ 'Silica'
Description: various small and unidentified silica phases are reported (sometimes associated with K-oxide)
ⓘ 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)
ⓘOsbornite1.BC.15TiN
ⓘSchreibersite1.BD.05(Fe,Ni)3P
Group 2 - Sulphides and Sulfosalts
ⓘTroilite2.CC.10FeS
ⓘAlabandite2.CD.10MnS
ⓘOldhamite2.CD.10CaS
ⓘDaubréelite2.DA.05Fe2+Cr3+2S4
Group 9 - Silicates
ⓘEnstatite9.DA.05Mg2Si2O6
ⓘClinoenstatite9.DA.10MgSiO3
ⓘAlbite9.FA.35Na(AlSi3O8)
ⓘvar. Oligoclase9.FA.35(Na,Ca)[Al(Si,Al)Si2O8]
Unclassified
ⓘ'Feldspar Group'-
ⓘ'Plagioclase'-(Na,Ca)[(Si,Al)AlSi2]O8
ⓘ'Silica'-
ⓘ'Nickel-iron'-

List of minerals for each chemical element

NNitrogen
Nⓘ OsborniteTiN
OOxygen
Oⓘ AlbiteNa(AlSi3O8)
Oⓘ ClinoenstatiteMgSiO3
Oⓘ EnstatiteMg2Si2O6
Oⓘ Albite var. Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
Oⓘ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
NaSodium
Naⓘ AlbiteNa(AlSi3O8)
Naⓘ Albite var. Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
Naⓘ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
MgMagnesium
Mgⓘ ClinoenstatiteMgSiO3
Mgⓘ EnstatiteMg2Si2O6
AlAluminium
Alⓘ AlbiteNa(AlSi3O8)
Alⓘ Albite var. Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
Alⓘ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
SiSilicon
Siⓘ AlbiteNa(AlSi3O8)
Siⓘ ClinoenstatiteMgSiO3
Siⓘ EnstatiteMg2Si2O6
Siⓘ Albite var. Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
Siⓘ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
PPhosphorus
Pⓘ Schreibersite(Fe,Ni)3P
SSulfur
Sⓘ AlabanditeMnS
Sⓘ DaubréeliteFe2+Cr23+S4
Sⓘ OldhamiteCaS
Sⓘ TroiliteFeS
CaCalcium
Caⓘ OldhamiteCaS
Caⓘ Albite var. Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
Caⓘ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
TiTitanium
Tiⓘ OsborniteTiN
CrChromium
Crⓘ DaubréeliteFe2+Cr23+S4
MnManganese
Mnⓘ AlabanditeMnS
FeIron
Feⓘ DaubréeliteFe2+Cr23+S4
Feⓘ Native IronFe
Feⓘ Native Iron var. Kamacite(Fe,Ni)
Feⓘ Schreibersite(Fe,Ni)3P
Feⓘ TroiliteFeS
NiNickel
Niⓘ Native Iron var. Kamacite(Fe,Ni)
Niⓘ Schreibersite(Fe,Ni)3P

Other Regions, Features and Areas containing this locality

AfricaContinent
African PlateTectonic Plate
North Africa
Northwest Africa MeteoritesGroup of Meteorite Fall Locations

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