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The Apennine Bench Formation revisitedThe Apennine Bench Formation consists of pre-mare light plains materials that crop out south of the crater Archimedes, inside the Imbrium basin. This material was ascribed to either impact or volcanic origins. The characteristics of Apollo 15 KREEP basalts and the Apennine Bench Formation are reviewed to determine whether their characteristics are compatible with a volcanic origin.
Document ID
19860013055
Acquisition Source
Legacy CDMS
Document Type
Conference Paper
Authors
Spudis, P. D. (Geological Survey Flagstaff, AZ, United States)
Hawke, B. R. (Hawaii Univ. Honolulu, United States)
Date Acquired
August 12, 2013
Publication Date
January 1, 1985
Publication Information
Publication: Lunar and Planetary Inst. Papers Presented to the Workshop on the Geology and Petrology of the Apollo 15 Landing Site
Subject Category
Lunar And Planetary Exploration
Accession Number
86N22526
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.

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