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Northwest Africa 14635 | |||||||||||||||||||||||||||||||
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Basic information | Name: Northwest Africa 14635 This is an OFFICIAL meteorite name. Abbreviation: NWA 14635 Observed fall: No Year found: 2009 Country: (Northwest Africa) Mass: 72 g | ||||||||||||||||||||||||||||||
Classification history: |
This is 1 of 4 approved meteorites classified as Achondrite (brachinite-like). [show all] Search for other: Primitive achondrites, Ungrouped achondrites | ||||||||||||||||||||||||||||||
Comments: | Approved 26 Mar 2022 | ||||||||||||||||||||||||||||||
Writeup |
Writeup from MB 111:
Northwest Africa 14635 (NWA 14635) (Northwest Africa) Purchased: 2009 Classification: Brachinite-like achondrite History: Purchased by Chalom Malka in 2009 from a meteorite dealer in Morocco. Physical characteristics: Three stones with weathered fusion crust. Petrography: (D. Sheikh, Cascadia) Sample displays a protogranular texture (Av. grain size=360±230 μm, n=253) predominantly composed of olivine (some grains are elongated and display a notable alignment) (~81 vol. %), orthopyroxene (some regions of the sample display orthopyroxene poikilitically enclosing olivine, chromite, and accessory plagioclase) (~15 vol. %), augite (~3 vol. %), chromite (~1 vol. %), and accessory plagioclase (observed only poikilitically enclosed within either orthopyroxene or chromite), troilite, chlorapatite, merrillite, and Fe-Ni metal (some altered to Fe-hydroxides). A fine-grained intergrowth of orthopyroxene + opaque minerals is observed along the margins of some olivine grains. Geochemistry: Olivine (Fa28.0±0.7, range Fa26.7-29.0, CaO=<0.1 wt. %, Cr2O3=<0.1 wt. %, Fe/Mg=0.39±0.01, Fe/Mn=54±2, n=17), Orthopyroxene (Fs23.9±1.5Wo1.9±0.5, range Fs20.5-24.7Wo0.8-2.2, Fe/Mn=36±3, n=13), Augite (Fs9.8±0.1Wo43.5±0.1, range Fs9.7-9.8Wo43.4-43.5, Al2O3=0.7±0.1 wt. %, Cr2O3=0.9±0.1 wt. %, Fe/Mn=25±2, n=2), Plagioclase (An35.2±0.8Or1.1±0.1, range An34.4-35.7Or1.1-1.2, n=3), Chromite (Cr#=76.1±0.1, Mg#=23.9±2.4, TiO2=1.3±0.1 wt. %, n=5). Classification: Achondrite (brachinite-like). While the overall texture, mineralogy, and mineral compositions of the sample are similar to brachinites, the high modal abundance of orthopyroxene, the presence of poikilitic pyroxene-rich areas, the near absence of plagioclase feldspar observed in the sample, the low abundance of CaO in olivine, the low Fe/Mg-Fe/Mn molar ratios of olivine, the fine-grained intergrowth of orthopyroxene + opaque minerals observed at olivine grain boundaries, and the more magnesian compositions of olivine and orthopyroxene indicate that this sample is representative of a brachinite-like achondrite (Goodrich et al., 2017), having similarities to NWA 595, NWA 1500, and NWA 5400. Specimens: 14.5 g at Cascadia, main mass with Chalom Malka | ||||||||||||||||||||||||||||||
Bibliography: |
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Data from: MB111 Table 0 Line 0: |
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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) |
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Catalogs: |
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References: | Published in Gattacceca J., McCubbin F. M., Grossman J. N., Schrader D. L., Chabot N. L., D’Orazio M., Goodrich C., Greshake A., Gross J., Joy K. H., Komatsu M. and Miao B. (2023) The Meteoritical Bulletin, No. 111. Meteoritics & Planetary Science 58, 901–904. ?
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Photos: |
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Geography: |
Statistics: This is 1 of 9921 approved meteorites from (Northwest Africa) (plus 1838 unapproved names) |