Lithologic components | Age (Ga) | Proportions at station 8 (%) | Modal percent plagioclase | Plagioclase composition | Fe/(Fe + Mg) in plagioclase |
---|---|---|---|---|---|
Mare basalt (92Â % high-Ti and 8Â % very-low-Ti basalts) | |||||
 High-Ti (HT) | 3.75 ± 0.01 to 3.85 ± 0.04 (1) | 25.8 | 23 (7) | An86-An87 (8) | 0.38 to 0.62 (8) |
 Very-low-Ti (VLT) | 3.63 ± 0.04 (2) | 2.2 | 32 (7) | An93-An96 (8) | 0.65 to 0.84 (8) |
 Orange glass (OG) | 3.60 ± 0.04 (3) to 3.66 ± 0.04 (4) | 12.0 | – | – |  |
Highland rocks | |||||
 Anorthositic norite (AN) | 3.75 ± 0.11 to 4.16 ± 0.04 (1) | 35.7 | 60–80 (9) | An85-An98 (9) | 0.44 to 1.00 (9) |
 Noritic breccia (NB) | 15.7 | 40–60 (9) | An86-An98 (9) | 0.19 to 1.00 (9) | |
 Mg-suite (60 % troctolite and 40 % norite) | |||||
 Mg-suite troctolite (Mg-T) | 4.46 ± 0.07 (5) to 4.18 ± 0.07 (6) | 4.62 | 60-85(10) | An94-An97 (11) | 0.44 to 1.00 (11) |
 Mg-suite norite (Mg-N) | 3.08 | 40-70(10) | An93-An94 (11) | 0.31 to 0.54 (11) |