Mathematics – Logic
Scientific paper
Dec 1975
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1975moon...14..491s&link_type=abstract
The Moon, vol. 14, Nov.-Dec. 1975, p. 491-504.
Mathematics
Logic
6
Apollo 17 Flight, Breccia, Lunar Evolution, Lunar Geology, Lunar Landing Sites, Astronomical Models, Chemical Composition, Impact Damage, Lunar Crust, Petrography, Radioactive Age Determination, Remanence
Scientific paper
A possible geological model for the origin and history of the materials that make up Boulder 1 is proposed on the basis of firm and probable regional, local, and boulder geological constraints. These constraints are described in detail, unresolved questions are considered, and a model is presented which appears to satisfy all the firm constraints and most of the probable constraints. According to this model, the crystallization of plagioclase and other ANT-suite phases now present in the boulder as clasts and matrix materials took place during the melted-shell stage of lunar history; the original rocks were greatly modified during the cratered-highland stage; and the events that determined the major characteristics of the boulder occurred during the large-basin stage.
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