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Northwest Africa 8418 | |||||||||||||||||||||||||||||||
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Basic information | Name: Northwest Africa 8418 This is an OFFICIAL meteorite name. Abbreviation: NWA 8418 Observed fall: No Year found: 2014 Country: (Northwest Africa) Mass: ![]() | ||||||||||||||||||||||||||||||
Classification history: |
This is 1 of 3 approved meteorites classified as C3. [show all] Search for other: Carbonaceous chondrites, Carbonaceous chondrites (type 3), and Ungrouped chondrites | ||||||||||||||||||||||||||||||
Comments: | Approved 27 May 2015 | ||||||||||||||||||||||||||||||
Writeup![]() |
Writeup from MB 104:
Northwest Africa 8418 (NWA 8418) (Northwest Africa) Purchased: 2014 Apr Classification: Carbonaceous chondrite (C3) History: Purchased by Darryl Pitt in April 2014 from a dealer in Erfoud, Morocco. Petrography: (A. Irving and S. Kuehner, UWS) Relatively fresh specimen composed of relatively large, separated granular chondrules in a finer grained metal-bearing matrix. Chlorapatite occurs throughout the matrix, along with Ni-poor kamacite, Ni-bearing lawrencite, Si-bearing Fe metal and rare merrillite. Some portions of this specimen contain large (up to 15.5 mm by 12 mm), ellipsoidal CAI consisting of porous aggregates (grainsize ~0.5 mm) of mainly Al-Ti-diopside, olivine and anorthite, with accessory spinel, troilite and taenite, surrounded by complete circumferential rims (~ 1 mm thick) of chlorapatite (each one rimmed in turn by a thin outer band of calcite). Phosphate and carbonate mineralogy was established by a combination of electron microprobe analysis and cathodoluminescence microscopy. Geochemistry: Olivine (Fa0.3-36.2; FeO/MnO = 130-131, N = 4), orthopyroxene (Fs1.9-2.3Wo1.0-0.9, N = 3), pigeonite (Fs1.7Wo9.5; Fs24.9Wo5.5), augite (Fs5.7Wo48.2), Al-Ti-diopside in CAI (Fs0.1Wo59.7; Al2O3 15.4 wt.%, TiO2 3.5 wt.%). Oxygen isotopes (K. Ziegler, UNM): analyses of three acid-washed subsamples by laser fluorination gave δ17O -3.994, -5.750, -5.299; δ18O 0.444, -1.773, -0.823; Δ17O -4.228, -4.814, -4.864. These values fall on the trend for CV and CK chondrites. Classification: Carbonaceous chondrite (C3) with affinities to CV chondrites. The abundance of apatite in this specimen is an anomalous feature for carbonaceous chondrites. Specimens: 22.2 g including one polished thin section at UWB. The remaining material is held by DPitt. | ||||||||||||||||||||||||||||||
Data from: MB104 Table 0 Line 0: |
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Plots: | O isotopes: | ||||||||||||||||||||||||||||||
Institutions and collections |
UNM: Institute of Meteoritics
MSC03 2050
University of New Mexico
Albuquerque NM 87131-1126
USA, United States; Website (institutional address; updated 12 Feb 2015) UWS: University of Washington, Department of Earth and Space Sciences, 70 Johnson Hall, Seattle, WA 98195, United States (institutional address; updated 15 Jan 2012) UWB: University of Washington, Box 353010 Seattle, WA 98195, United States (institutional address; updated 27 Jul 2012) DPitt: Darryl Pitt, 225 West 83rd Street, New York, NY 10024, United States; Website (private address) |
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Catalogs: |
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References: | Published in Meteoritical Bulletin, no. 104, MAPS 52, 2284, Octover 2017, http://onlinelibrary.wiley.com/doi/10.1111/maps.12930/full
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Geography: |
Statistics: This is 1 of 9013 approved meteorites from (Northwest Africa) (plus 1869 unapproved names) |