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Late Influx: Evidence from Siderophile Elements in Terrestrial Peridotites and Lunar BrecciasIn terrestrial peridotites, Pd is sometimes enhanced relative to other PGE. This observation is taken to imply a "non-chondritic" HSE signature in the mantle. A similar pattern is seen in some Apollo 17 breccias suggesting it to be a primordial feature of late influx. Additional information is contained in the original extended abstract.
Document ID
20010044936
Document Type
Conference Paper
Authors
Morgan, J. W.
(Maryland Univ. College Park, MD United States)
Brandon, A. D.
(Maryland Univ. College Park, MD United States)
Walker, R. J.
(Maryland Univ. College Park, MD United States)
Horan, M. F.
(Carnegie Institution of Washington Washington, DC United States)
Date Acquired
August 20, 2013
Publication Date
January 1, 2001
Publication Information
Publication: Lunar and Planetary Science XXXII
Subject Category
Lunar And Planetary Science And Exploration
Funding Number(s)
CONTRACT_GRANT: NAG5-7634
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.

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