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X-Ray Diffraction Study of L2005 AG17 (IDPs) by Using SRX-ray diffraction study revealed the existence of magnetite and new type of pyrrhotite with the chemical formula of Fe0.56S in L2005 AG17. Considering the total chemical formula of Fe0.83S, residual iron in amorphous state might exist in this sample. Additional information is contained in the original extended abstract.
Document ID
20020046012
Acquisition Source
Johnson Space Center
Document Type
Conference Paper
Authors
Ohsumi, K. O.
(High Energy Accelerator Research Organization Tsukuba, Japan)
Hagiya, K. H.
(NASA Johnson Space Center Houston, TX United States)
Zolensky, M. E.
(NASA Johnson Space Center Houston, TX United States)
Date Acquired
August 20, 2013
Publication Date
April 1, 2002
Publication Information
Publication: Lunar and Planetary Science XXXIII
Subject Category
Lunar And Planetary Science And Exploration
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.

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