HI ALL
 i have sale thnis specimen, of nwa 5790 nakhlite unique structure and not 
paied to any other martian nakhlite

this 63.4 gr,


http://www.flickr.com/photos/azizhabibi/4138934360/
 http://www.flickr.com/photos/azizhabibi/4138168819/
http://www.flickr.com/photos/azizhabibi/4138167219/


please maker me your offer ,  and if you are interetsed in small fragment send 
me an email i may break it in small fragment,
so i need a list of potential buyers of small fragments

thanks
aziz habibi
http://tin.er.usgs.gov/meteor/metbull.php?code=49470
Northwest Africa 5790 
Basic information Name: Northwest Africa 5790
     This is an OFFICIAL meteorite name.
Abbreviation: NWA 5790 
Observed fall: No
Year found: 2009
Country: (Northwest Africa) 
Mass: 145 g
 
Classification
  history: Recommended:     Martian (nakhlite)    [explanation] 

: Planetary meteorites, Martian meteorites
 
Comments: Approved 29 Nov 2009 
Writeup Writeup from MB 97: 
Northwest Africa 5790
Erfoud, Morocco
Find: spring 2009
Classification: Martian (nakhlite)
History: Found in the desert by nomads and purchased by A. Habibi in Erfoud 
(Morocco). 
Physical characteristics: Two stones for a TKW of 145 g, with mm-sized 
phenocrysts in a groundmass with pinkish luster. Very friable.
Petrography: (A. Jambon, O. Boudouma, D. Badia, UPVI ) Dominated by mm-sized 
euhedral augite with sharp rim zoning and faint irregular zoning inside. 
Subsidiary euhedral olivine phenocrysts are of similar size, zoned to their 
core. Interstitial mesostasis contains dendritic oxides, pyroxene, feldspar, 
silica, phosphate and glass. Minor Cl-amphiboles in trapped melt inclusions. 
Mode from BSE images: augite 51.2, olivine 9.1, mesostasis 39.7, 
titanomagnetite <1%.
Mineral compositions (SEM and EMPA; as above) and geochemistry (ICP-MS; J-A 
Barrat UBO): zoned augite core (En35Fs24Wo40 and Fe/Mn = 32) sharp rim  
(En20Fs43Wo36 and Fe/Mn = 42), olivine progressively zoned from the core (Fa65 
with Fe/Mn = 47) to the rim (Fa80 with Fe/Mn = 40). Rare Ti-magnetite 
phenocrysts. Uv32Mt56Sp7Ct4 with fine ilmenite exsolutions. In the mesostasis, 
dendritic crystals of Ti Magnetite: Uv52-74Mt38-19, acicular pyroxene  
(En7Fs47Wo46 and Fe/Mn = 55) and olivine Fa88. Plagioclase An16Ab79Or5. Augite 
with 2-3 wt% Cl.
Bulk major-element chemistry:  similar to other nakhlites; element ratios 
confirm Martian origin (K/La =473, Ga/Al =3.7 104 [sic]); significantly higher 
proportion of mesostasis than other nakhlites with the highest Th, U and rare 
earth elements (REE) concentrations ever reported for a nakhlite (e.g. , Th = 
0.85 ppm); REE pattern characterized by a strong light REE enrichment (La/Yb)n 
= 5.8, and Eu/Eu* = 0.86. 
Oxygen isotopes (R. Greenwood and I. Franchi, OU ): ∆17O = 0.30‰. 
Type specimens: A total sample mass of 16 g is on deposit at UPVI ; 2.77 g 
UAlberta; 1.25g UWS ; main mass, Habibi.


      
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