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    Internal structure of type I deep-sea spherules by X-ray computed microtomography

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    Author
    Feng, H.
    Jones, K. W.
    Tomov, S.
    Stewart, B.
    Herzog, G. F.
    Schnabel, C.
    Brownlee, D. E.
    Issue Date
    2005-01-01
    Keywords
    tomography
    micrometeorites
    Deep-sea spherules
    
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    Citation
    Feng, H., Jones, K. W., Tomov, S., Stewart, B., Herzog, G. F., Schnabel, C., & Brownlee, D. E. (2005). Internal structure of type I deep‐sea spherules by X‐ray computed microtomography. Meteoritics & Planetary Science, 40(2), 195-206.
    Publisher
    The Meteoritical Society
    Journal
    Meteoritics & Planetary Science
    URI
    http://hdl.handle.net/10150/655961
    DOI
    10.1111/j.1945-5100.2005.tb00375.x
    Additional Links
    https://meteoritical.org/
    Abstract
    The internal structures of type I spherules (melted micrometeorites rich in iron) have been investigated using synchrotron-based computed microtomography. Variations from sphericity are smallthe average ratio of the largest to the smallest semimajor axis is 1.07 +/- 0.06. The X-ray tomographs reveal interior cavities, four spherules with metal cores with diameters ranging from 57 to 143 micrometers and, in two spherules, high attenuation features thought to be nuggets rich in platinumgroup elements. Bulk densities range from 4.2 to 5.9 g/cm3 and average grain densities from 4.5 to 6.5 (g/cm3) with uncertainties of 10-15%. The average grain densities are those expected for materials containing mostly oxides of iron and nickel. The tomographic density measurements indicate an average void space of 5 +8/-5%. The void spaces may be contraction features or the skeletons of bubbles that formed in the molten precursors during atmospheric passage.
    Type
    Article
    text
    Language
    en
    ISSN
    1945-5100
    ae974a485f413a2113503eed53cd6c53
    10.1111/j.1945-5100.2005.tb00375.x
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    Meteoritics & Planetary Science, Volume 40, Number 2 (2005)

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