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Itqiy meteorite, al-Saqiyah al-Hamra'a (Saguia el Hamra), Western Saharai
Regional Level Types
Itqiy meteoriteMeteorite Fall Location
al-Saqiyah al-Hamra'a (Saguia el Hamra)Wadi
Western SaharaDisputed Territory

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Latitude & Longitude (WGS84):
26° 35' 26'' North , 12° 57' 7'' West
Latitude & Longitude (decimal):
Köppen climate type:


Primitive Enstatite Achondrite [or Shock-melted Enstatite Chondrite]
1990 fall. 2 pieces, 410g and 4310g.

After a striking burst of light-and-sound, a 410 g stone was recovered by a nomad. A decade later a 4.31 kg stone was recovered — and the news of Itqiy spread.

The dominant constituent of Itqiy is enstatite accompanied by kamacite (~ 25 vol%) and tiny kamacite-sulfide intergrowths. The very reduced mineralogy, the oxygen isotopes, and the cosmic ray exposure age all indicate that Itqiy is a member of the Enstatite-rich meteorite clan, initially described as an Enstatite chondrite, but beyond that classification is elusive. The enstatite resembles that of EL chondrites, but the metal is closer in composition to that of EH chondrites. Furthermore, Itqiy lacks chondrules and chondrule relics. This may be entirely due to impact melting from pre-terrestrial shock, but that is a hypothesis — not a conclusion. To begin with, there is apparently no consensus on the level of shock.

The actual issues are deeper than that. Over two decades ago Klaus Keil (1989) argued that the Enstatite meteorites were derived from a minimum of four parent bodies (EH and EL chondrites, normal aubrites, and the Shallowater parent body). Recently, however, it has become increasingly difficult to accommodate several Enstatite meteorites into the four homeworld framework. Worlds that have been completely melted (e.g., Happy Canyon, Itqiy, NWA 2526) are especially difficult to understand. First, disentangling the effects of internally generated metamorphism from external shock(s) is difficult. Secondly, it is not clear whether all of the Enstatite-rich oddballs are derived from the four putative homeworlds. Recently, Keil and Bischoff (2008) have proposed that Itqiy and NWA 2526 may be derived from a fifth parent body.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


9 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
Reference: Patzer, A., Hill, D. H., & Boynton, W. V. (2001). Itqiy: A metal‐rich enstatite meteorite with achondritic texture. Meteoritics & Planetary Science, 36(11), 1495-1505.
Daubréelite
Formula: Fe2+Cr3+2S4
Reference: Patzer, A., Hill, D. H., & Boynton, W. V. (2001). Itqiy: A metal‐rich enstatite meteorite with achondritic texture. Meteoritics & Planetary Science, 36(11), 1495-1505.
Enstatite
Formula: Mg2Si2O6
Reference: Patzer, A., Hill, D. H., & Boynton, W. V. (2001). Itqiy: A metal‐rich enstatite meteorite with achondritic texture. Meteoritics & Planetary Science, 36(11), 1495-1505.
Iron
Formula: Fe
Reference: Patzer, A., Hill, D. H., & Boynton, W. V. (2001). Itqiy: A metal‐rich enstatite meteorite with achondritic texture. Meteoritics & Planetary Science, 36(11), 1495-1505.
Iron var. Kamacite
Formula: (Fe,Ni)
Reference: Patzer, A., Hill, D. H., & Boynton, W. V. (2001). Itqiy: A metal‐rich enstatite meteorite with achondritic texture. Meteoritics & Planetary Science, 36(11), 1495-1505.
Niningerite
Formula: (Mg,Fe2+,Mn2+)S
Reference: Patzer, A., Hill, D. H., & Boynton, W. V. (2001). Itqiy: A metal‐rich enstatite meteorite with achondritic texture. Meteoritics & Planetary Science, 36(11), 1495-1505.
Oldhamite
Formula: (Ca,Mg)S
Reference: Patzer, A., Hill, D. H., & Boynton, W. V. (2001). Itqiy: A metal‐rich enstatite meteorite with achondritic texture. Meteoritics & Planetary Science, 36(11), 1495-1505.
Perryite ?
Formula: (Ni,Fe)5(Si,P)2
Reference: Patzer, A., Hill, D. H., & Boynton, W. V. (2001). Itqiy: A metal‐rich enstatite meteorite with achondritic texture. Meteoritics & Planetary Science, 36(11), 1495-1505.
Schreibersite ?
Formula: (Fe,Ni)3P
Reference: Patzer, A., Hill, D. H., & Boynton, W. V. (2001). Itqiy: A metal‐rich enstatite meteorite with achondritic texture. Meteoritics & Planetary Science, 36(11), 1495-1505.
Troilite
Formula: FeS
Reference: Patzer, A., Hill, D. H., & Boynton, W. V. (2001). Itqiy: A metal‐rich enstatite meteorite with achondritic texture. Meteoritics & Planetary Science, 36(11), 1495-1505.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Iron1.AE.05Fe
var. Kamacite1.AE.05(Fe,Ni)
Perryite ?1.BB.10(Ni,Fe)5(Si,P)2
Schreibersite ?1.BD.05(Fe,Ni)3P
Group 2 - Sulphides and Sulfosalts
Alabandite2.CD.10MnS
Daubréelite2.DA.05Fe2+Cr3+2S4
Niningerite2.CD.10(Mg,Fe2+,Mn2+)S
Oldhamite2.CD.10(Ca,Mg)S
Troilite2.CC.10FeS
Group 9 - Silicates
Enstatite9.DA.05Mg2Si2O6

List of minerals for each chemical element

OOxygen
O EnstatiteMg2Si2O6
MgMagnesium
Mg EnstatiteMg2Si2O6
Mg Oldhamite(Ca,Mg)S
Mg Niningerite(Mg,Fe2+,Mn2+)S
SiSilicon
Si EnstatiteMg2Si2O6
Si Perryite(Ni,Fe)5(Si,P)2
PPhosphorus
P Schreibersite(Fe,Ni)3P
P Perryite(Ni,Fe)5(Si,P)2
SSulfur
S Oldhamite(Ca,Mg)S
S Niningerite(Mg,Fe2+,Mn2+)S
S DaubréeliteFe2+Cr23+S4
S TroiliteFeS
S AlabanditeMnS
CaCalcium
Ca Oldhamite(Ca,Mg)S
CrChromium
Cr DaubréeliteFe2+Cr23+S4
MnManganese
Mn Niningerite(Mg,Fe2+,Mn2+)S
Mn AlabanditeMnS
FeIron
Fe Iron var. Kamacite(Fe,Ni)
Fe Niningerite(Mg,Fe2+,Mn2+)S
Fe DaubréeliteFe2+Cr23+S4
Fe TroiliteFeS
Fe IronFe
Fe Schreibersite(Fe,Ni)3P
Fe Perryite(Ni,Fe)5(Si,P)2
NiNickel
Ni Iron var. Kamacite(Fe,Ni)
Ni Schreibersite(Fe,Ni)3P
Ni Perryite(Ni,Fe)5(Si,P)2

References

Sort by

Year (asc) Year (desc) Author (A-Z) Author (Z-A)
Keil, K. (1989) Enstatite meteorites and their parent bodies, Meteoritics: 24(4): 195-208.
Patzer, A. et al. (2001) Itqiy: II. a Short Story About Its Noble Gases and Oxygen Isotopes. Meteoritics & Planetary Science: 36 (Supplement): A158.
Grossman, J.N., Zipfel, J. (2001) The Meteoritical Bulletin: 85: Meteoritics & Planetary Science: 36 (Supplement): A293-A322.
Patzer, A., Hill, D.H., Boynton, W.V. (2001) Itqiy: A metal‐rich enstatite meteorite with achondritic texture. Meteoritics & Planetary Science: 36(11): 1495-1505.
Keil, K., Adolf Bischoff, A. (2008) Northwest Africa 2526: A partial melt residue of enstatite chondrite parentage. Meteoritics & Planetary Science: 43(7): 1233-1240.
Niekerk, D., Keil, K., Humayun, M. (2014) Petrogenesis of anomalous Queen Alexandra Range enstatite meteorites and their relation to enstatite chondrites, primitive enstatite achondrites, and aubrites. Meteoritics & Planetary Science, Online Early.

Other Databases

Wikipedia:https://en.wikipedia.org/wiki/Itqiy_meteorite
Wikidata ID:Q1449768

External Links


Other Regions, Features and Areas containing this locality

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

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