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Lut 003
Basic information Name: Lut 003
     This is an OFFICIAL meteorite name.
Abbreviation: There is no official abbreviation for this meteorite.
Observed fall: No
Year found: 2013
Country: Iran
Mass:help 505 g
Classification
  history:
Meteoritical Bulletin:  MB 103  (2014)  L3
Recommended:  L3    [explanation]

This is 1 of 680 approved meteorites classified as L3.   [show all]
Search for other: L chondrites, L chondrites (type 3), Ordinary chondrites, and Ordinary chondrites (type 3)
Comments: Approved 11 Jul 2014
Writeuphelp
Writeup from MB 103:

Lut 003        30°16’21"N, 59°21’23"E

Kerman, Iran

Found: 2013 Mar 21

Classification: Ordinary chondrite (L3)

History: A single stone found during an expedition in the Lut desert of Iran, on sand dunes known to locals as Rig-e Yalan. Two pieces totalling 25.8 g were donated to Cascadia on May 1, 2013.

Physical characteristics: Physical: Cut face shows a medium to dark brown interior with very little visible metal or sulfide. A few lighter colored chondrules are visible in hand specimen. White secondary mineralization is visible in one fracture. Exterior is covered by a dark brown weathering patina cut across by dark-colored fractures.

Petrography: (M. Hutson and A. Ruzicka, Cascadia). The meteorite is heavily brecciated on the scale of individual chondrules; clearly defined chondrules are relatively rare. Finer-grained areas consist of smaller chondrule and mineral fragments. Abundant low-calcium clinopyroxene is easily observed in cross-polarized light. The meteorite is crossed by numerous weathering veins. In thin section, approximately 60-70% of the metal and troilite has been converted to weathering product. Total opaques (weathering product + troilite + rare metal) comprise between 5 to 10% of the meteorite. Diameters of 31 chondrules/chondrule fragments average 620 μm.

Geochemistry: Compositions of measured phases are variable, and include olivine Fa18.7±8.2 (median Fa19.7) (N=25), and low-Ca pyroxene Wo1.1±0.65Fs16.1±6.1En82.8±6.4 (N=16).

Classification: A fragmental L3 chondrite is suggested by texture, mineral chemistry, chondrule size, and abundance of opaque minerals.

Specimens: Two pieces (19.0 and 3.8 g), one polished thin section, and a stub are on deposit at Cascadia. Mr. Maziar Nazari and Mr. Kiyan Babazadeh hold the main mass (PO Box 17665-414, Tehran, Iran).

Data from:
  MB103
  Table 0
  Line 0:
State/Prov/County:Kerman
Origin or pseudonym:sand dunes
Date:2013 Mar 21
Latitude:30°16'21"N
Longitude:59°21'23"E
Mass (g):504.5
Pieces:1
Class:L3
Shock stage:S3
Weathering grade:W3
Fayalite (mol%):18.7±8.2
Ferrosilite (mol%):16.1±6.1
Wollastonite (mol%):1.1±0.7
Classifier:M. Hutson and A. Ruzicka, Cascadia
Type spec mass (g):22.8
Type spec location:Cascadia
Main mass:Mr. Maziar Nazari and Mr. Kiyan Babazadeh
Finder:Mazier Nazari, Kiyan Babazadeh, Ashkan Hedayati, Mohsen Adib
Comments:Lab number CML0741, field number Lut #504.5; submitted by Alex Ruzicka
Institutions
   and collections
Cascadia: Cascadia Meteorite Laboratory, Portland State University, Department of Geology, Room 17 Cramer Hall, 1721 SW Broadway, Portland, OR 97201, United States; Website (institutional address; updated 28 Oct 2011)
Catalogs:
References: Published in Meteoritical Bulletin, no. 103, MAPS 52, 1014, May 2017, http://onlinelibrary.wiley.com/doi/10.1111/maps.12888/full
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Geography:

Iran
Coordinates:
     Recommended::   (30° 16' 21"N, 59° 21' 23"E)

Statistics:
     This is 1 of 244 approved meteorites from Kerman, Iran
     This is 1 of 262 approved meteorites from Iran (plus 46 unapproved names)
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