Ph. Warren, A CONCISE COMPILATION OF PETROLOGIC INFORMATION ON POSSIBLY PRISTINE NONMARE MOON ROCKS, The American mineralogist, 78(3-4), 1993, pp. 360-376
To facilitate systematic study of the surviving compositionally pristi
ne (endogenously igneous) rocks of the ancient lunar crust, a compilat
ion has been generated of all likely samples, along with key informati
on on the petrologic characteristics and chemistry of each sample. The
compilation includes 260 samples. Besides information related to the
likelihood of each sample being truly pristine (i.e., mainly its textu
re and siderophile element abundances), information is compiled on min
eral content, listing major phases present as well as basic informatio
n on mineral compositions, on size (expressed as mass), and on whether
a reasonably comprehensive chemical analysis has been published. The
compilation also classifies the samples into seven categories of confi
dence in the pristine composition of the samples, reflecting an estima
tion of the relative likelihood that each arguably pristine sample is
in fact pristine. For many purposes, it is crucial to avoid inclusion
of polymict rocks in a data base. On petrologic diagrams such as a plo
t of average Mg' [Mg' = 100 x molar Mg/(Mg + Fe)] in a low-Ca mafic si
licate vs. average An content in plagioclase, rocks in the top three c
ategories of the confidence in pristine character appear distinctly bi
modal in composition, with roughly half belonging to a ferroan suite c
haracterized by high An despite relatively low Mg'. When samples of lo
w to moderate pristine character are included, the bimodality appears
less distinct. Sample mass can also be important. With a data base res
tricted to samples more massive than 1 g, there is a clear distinction
in feldspar content and bulk density between ferroan and nonferroan (
Mg-suite) rocks, such that only the ferroan-suite rocks are likely to
have formed as flotation cumulates. With a data base including smaller
samples, the same basic pattern is seen, but only in a blurred form,
as the two rock types show considerable overlap in their modal feldspa
r contents.