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1 History  





2 Mineralogy and petrology  





3 Classification  





4 Parent body  





5 See also  





6 References  














Itqiy meteorite






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Coordinates: 26°3527N 12°578W / 26.59083°N 12.95222°W / 26.59083; -12.95222
 

From Wikipedia, the free encyclopedia
 


This is an old revision of this page, as edited by Meteoritekid (talk | contribs)at11:39, 14 July 2020 (Classification). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.
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Itqiy meteorite
TypeChondrite (ongoing scientific debate)
ClassEnstatite chondrite (ongoing scientific debate)
GroupEH7-an (ongoing scientific debate)
Parent bodyNWA2526-Itqiy[1]
CompositionEnstatite (78 %), meteoric iron (22 %), sulfides.[2]
CountryWestern Sahara[3]
Coordinates26°35′27N 12°57′8W / 26.59083°N 12.95222°W / 26.59083; -12.95222[3]
Observed fallYes[3]
Fall date1990[3]
Found date1990 + 2000-07[3]
TKW0.410 kilograms (0.90 lb)[3] + 4.310 kilograms (9.50 lb)[3]

The Itqiy meteorite is an enstatite-rich stony-iron meteorite. It is classified as an enstatite chondrite of the EH group that was nearly melted and is therefore very unusual for that group.[2][4] Other classifications have been proposed and are an ongoing scientific debate.

History

Itqiy was initially attributed to a 1990 fireball in Western Sahara. One stone was recovered by a nomad, and a second stone was recovered in July 2000 by Marc, Luc, and Jim Labenne who were searching for meteorites in the same location.[3] The meteorite was analyzed in 2001.[5] Later work showed that the meteorite had fallen nearly 6,000 years ago and was not associated with any recent fireball. [6]

Mineralogy and petrology

Itqiy is a stony meteorite consisting of 78% enstatite and 22% meteoric iron. The meteoric iron is kamacite with 5.77% nickel. Small amounts of other minerals include troilite, Mg-Mn-Fe sulfides and Fe-Cr sulfides.[2][7]

Classification

The meteorite was described as an "ungrouped stony meteorite" in 2000, and reclassified as an "ungrouped enstatite meteorite" in 2001.[2][7] In 2006, Itqiy was classified as a member of the EH enstatite chondrites, with a petrologic type of 7, emphasizing that it was a strongly metamorphosed EH chondrite.[2]

Itqiy represents a rock that formed through partial melting of an EH chondrite. This process removed the more volatile minerals like plagioclase.[8] In 2011 it was proposed that Itqiy, QUE 94204, QUE 97289, QUE 97348, NWA 2526 and possibly Yamato 793225 are part of a new group that should be called "primitive enstatite achondrites".[9]

Parent body

In 2010 it was proposed that NWA 2526 and Itqiy share the same parent body.[8]

See also

References

  1. ^ Keil, Klaus (31 December 2009). "Enstatite achondrite meteorites (aubrites) and the histories of their asteroidal parent bodies". Chemie der Erde - Geochemistry. 70 (4): 295–317. Bibcode:2010ChEG...70..295K. doi:10.1016/j.chemer.2010.02.002.
  • ^ a b c d e "Itqiy". Meteoritical Society.
  • ^ a b c d e f g h "Itqiy". Meteoritical Society. Retrieved 21 December 2012.
  • ^ "EH7-an". Meteoritical Society.
  • ^ Grossman, Jeffrey N.; Jutta Zipfel (2001). "The Meteoritical Bulletin, No. 85, 2001 September" (PDF). Meteoritics & Planetary Science. 36: A293–A322. Bibcode:2001M&PS...36..293G. doi:10.1111/j.1945-5100.2001.tb01542.x. Retrieved 21 December 2012.
  • ^ {{cite journal|last=Patzer|first=Andrea|author2=Dolores Hill|author3=William Boynton|author4=Luitgard Franke|author5=Ludolf Schultz|author6=Timothy Jull|author7=Lanny McHargue|author8=Ian Franchi|title=Itqiy: A study of noble gases and oxygen isotopes including its terrestrial age and a comparison with Zakłodzie|journal=Meteoritics & Planetary Science|date=2010|volume=37|pages=823–833|doi=10.1111/j.1945-5100.2002.tb00858.x |url=https://onlinelibrary.wiley.com/doi/abs/10.1111/j.1945-5100.2002.tb00858.x%7Caccessdate=14 July 2020}
  • ^ a b Patzer, Andrea; Hill, Dolores H.; Boynton, William V. (1 November 2001). "Itqiy: A metal-rich enstatite meteorite with achondritic texture". Meteoritics & Planetary Science. 36 (11): 1495–1505. Bibcode:2001M&PS...36.1495P. doi:10.1111/j.1945-5100.2001.tb01841.x.
  • ^ a b Keil, Klaus (2010). "Enstatite achondrite meteorites (aubrites) and the histories of their asteroidal parent bodies". Chemie der Erde - Geochemistry. 70 (4): 295–317. Bibcode:2010ChEG...70..295K. doi:10.1016/j.chemer.2010.02.002.
  • ^ IZAWA, Matthew R. M.; FLEMMING, Roberta L.; BANERJEE, Neil R.; MATVEEV, Sergei (1 November 2011). "QUE 94204: A primitive enstatite achondrite produced by the partial melting of an E chondrite-like protolith". Meteoritics & Planetary Science. 46 (11): 1742–1753. Bibcode:2011M&PS...46.1742I. doi:10.1111/j.1945-5100.2011.01263.x.

  • Retrieved from "https://en.wikipedia.org/w/index.php?title=Itqiy_meteorite&oldid=967635640"

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    This page was last edited on 14 July 2020, at 11:39 (UTC).

    This version of the page has been revised. Besides normal editing, the reason for revision may have been that this version contains factual inaccuracies, vandalism, or material not compatible with the Creative Commons Attribution-ShareAlike License.



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