12016 contains resorbed olivine crystals often included within pyroxene grains. Pyroxenes tend to be elongate (0.5 to 1 mm) and occur as complex intergrowths of augite and pigeonite. Plagioclase occurs interstitially, and is sometimes subpoikililitic. The groundmass of 12016 includes grains of fayalite, silica and phosphate in a cryptocrystalline matrix of devitrified glass.
The sample weighed 2028.3 grams before analysis. It has not been dated.
Further details of this and other Apollo samples are here: http://curator.jsc.nasa.gov
Apollo 12 returned 34 kilograms of samples, including 45 rocks, samples of lunar 'soil', and several core tubes that included material from as much as 40 centimetres below the lunar surface.
Apollo 12 rocks were almost all basalts, with only two breccias in the returned samples. The basalts at the Apollo 12 site formed 3.1 to 3.3 billion years ago, roughly 500 million years later than the Apollo 11 basalts. Overall, there is much less of the element titanium in the Apollo 12 samples than in the Apollo 11 samples, which explains the more reddish colour of this region. The differences in age and chemical composition between the Apollo 11 and Apollo 12 samples demonstrate that mare volcanism did not occur as a single, Moon-wide melting event.
Apollo 12 was launched on 14 November 1969.