Meteoritic material in lunar highland samples from the Apollo 11 and 12 sitesRadiochemical neutron activation analyses for Ag, Au, Bi, Br, Cd, Cs, Ge, In, Ir, Ni, Os, Pd, Rb, Re, Sb, Te, Tl, U and Zn were carried out on 11 samples from the Apollo 11 and 12 sites (two samples of rock 12013, one granitic and one KREEPy; 4 KREEP fragments from 2-4 mm soil 12033,2; 4 anorthositic fragments from 1-3 mm soil 10085,104; 1 sample of 'Luny' rock-felsite-KREEP breccia 12013 10085,31 LR-1). Most Apollo 12 samples were found to have an Imbrium meteoritic component; others, typified by the Luny breccia, apparently contain a new meteoritic component of low Re content. Components of higher Ir/Au ratio (3L, 5L and 7) were found in Apollo 11 anorthositic samples; the fact that their enrichment in meteoritic siderophiles parallels that of Fe, Mg, REE and other KREEP elements is consistent with progressive contamination of an anorthositic crust. The Luny rock was tentatively classified Group 2, supporting the assignment of this group to Serenitatis.
Document ID
19790055169
Acquisition Source
Legacy CDMS
Document Type
Conference Proceedings
Authors
Janssens, M.-J. (Chicago Univ. Chicago, IL, United States)
Hertogen, J. (Chicago, University Chicago, Ill.; Gent, Rijksuniversiteit, Ghent, Belgium)
Palme, H. (Chicago Univ. Chicago, IL, United States)
Anderson, A. T. (Chicago Univ. Chicago, IL, United States)
Anders, E. (Chicago, University Chicago, Ill., United States)