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Meteorite NWA 11448 - Primitive Achondrite Ureilite - Fragment 14.47g

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    Description

    NWA 11448
    NWA 11448
    Found Sahara, 2017
    Primitive Achondrite
    Ureilite
    Specimen is a 14.47g fragment, as found
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    Olivine (~70 vol.%) and Pigeonite (~30 vol.%) exhibiting
    some preferred shape orientation
    A technical name for ureilite would be olivine-pigeonite achondrite. Compared to most other meteorites,
    ureilites tend to have a high percentage of carbon (average 3% by weight) in the form of graphite and nanodiamonds.
    The diamonds, which are rarely more than a few micrometres in diameter, are probably the result of high pressure shockwaves produced by collisions of the ureilite parent body with other asteroids.
    A recent study
    (
    Carbon isotopic variation in ureilites: Evidence for an early, volatile-rich Inner Solar System
    ; Jean-Alix Barrat, Pierre Sansjofre, Akira Yamaguchi, Richard C.Greenwood, Philippe Gillet
    ), suggest the Ureilite Parent Body was an at least 690km size "planetoid" of the early Inner Solar System.
    From the Meteoritical society Database :
    Northwest Africa 11448
    Basic information
    Name:
    Northwest Africa 11448
    This is an OFFICIAL meteorite name.
    Abbreviation:
    NWA 11448
    Observed fall:
    No
    Year found:
    2017
    Country:
    (Northwest Africa)
    Mass:
    62.7 g
    Classification
    history:
    Recommended:
    Ureilite
    [explanation]
    This is 1 of 437 approved meteorites classified as Ureilite.
    Comments:
    Approved 30 Oct 2017
    Writeup
    Writeup from MB 106:
    Northwest Africa 11448
    (NWA 11448)
    (Northwest Africa)
    Purchased: 2017 Apr
    Classification: Ureilite
    History
    : Purchased by Fabien
    Kuntz
    in April 2017 from a dealer in Erfoud, Morocco.
    Petrography
    : (A. Irving and S. Kuehner,
    UWS
    ) Aggregate of elongate grains of olivine (~70 vol.%) and pigeonite (~30 vol.%) exhibiting some preferred shape orientation, plus interstitial finer grained, dark brown zones. Olivine has reduced magnesian rims associated with blebby Fe metal.
    Geochemistry
    : Olivine (cores Fa
    22.4-22.6
    ; rim Fa
    11.8
    ; N = 3), pigeonite (Fs
    17.7-18.0
    Wo
    10.3-10.1
    , N = 2).
    Classification
    : Ureilite.
    Specimens
    : 12.86 g including one polished thin section at
    PSF
    ; remainder with
    Kuntz
    .
    Data from:
    MB106
    Table 0
    Line 0:
    Place of purchase:
    Erfoud
    Date:
    P 2017 Apr
    Mass (g):
    62.7
    Pieces:
    1
    Class:
    Ureilite
    Shock stage:
    moderate
    Weathering grade:
    low
    Fayalite (mol%):
    22.4-22.6; 11.8
    Ferrosilite (mol%):
    17.7-18.0
    Wollastonite (mol%):
    10.3-10.1
    Classifier:
    A. Irving and S. Kuehner, UWS
    Type spec mass (g):
    12.86
    Type spec location:
    PSF
    Main mass:
    F. Kuntz
    Comments:
    Work name K339; submitted by A. Irving
    Institutions
    and collections
    PSF
    : Planetary Studies Foundation,10 Winterwood Lane, Unit B, Galena, Illinois 61036-9283, United States;
    Website
    (institutional address; updated 1 Dec 2011)
    UWS
    : University of Washington, Department of Earth and Space Sciences, 70 Johnson Hall, Seattle, WA 98195, United States (institutional address; updated 15 Jan 2012)
    Kuntz
    : Fabien Kuntz, France;
    Website
    (private address)
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