Table 1 Model input parameters and resulting melt volume, temporal, and spatial data
From: Rapid transition from primary to secondary crust building on the Moon explained by mantle overturn
Model input | Melt Vol. (% crust) | FWHM (My) | Magmatic timing (My) | Farthest neighbor (⨴) + Exposure prop. (⨵) = ⨷ | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
Model | IBC (km) | Ƞ contrast | Ref. Ƞ (Pa s) | 2% | 3% | 4% | 5% | 6% | 7% | |||
Run 1 | 30 | 10-1 | 5 × 1020 | 8.2 | 69.2 | 155.9 | ⨴ | ⨴ | ⨷ | ⨴ | ⨴ | |
Run 2 | 30 | 10-2 | 1021 | 5.6 | 37.1 | 92.4 | ⨴ | ⨷ | ⨴ | |||
Run 3 | 30 | 10-2 | 5 × 1020 | 8.4 | 10.5 | 37.1 | ⨴ | ⨴ | ⨷ | ⨴ | ⨴ | |
Run 4 | 30 | 10-3 | 1021 | 10.0 | 10.6 | 35.6 | ⨴ | ⨷ | ⨴ | ⨴ | ⨴ | |
Run 5 | 30 | 10-3 | 5 × 1020 | 6.9 | 2.5 | 14.7 | ⨴ | ⨴ | ⨷ | ⨴ | ⨴ | |
Run 6 | 50 | 10−2 | 1021 | 13.2 | 20.2 | 55.6 | ⨴ | ⨴ | ⨷ | ⨴ | ⨴ | ⨴ |
Run 7 | 50 | 10-2 | 5 × 1020 | 17.0 | 7.8 | 25.3 | ⨴ | ⨴ | ⨷ | ⨷ | ⨴ | ⨴ |
Run 8 | 50 | 10−3 | 1021 | 15.3 | 7.1 | 23.4 | ⨴ | ⨴ | ⨷ | ⨷ | ⨴ | ⨴ |
Run 9 | 50 | 10-3 | 5 × 1020 | 17.2 | 3.5 | 12.1 | ⨴ | ⨴ | ⨷ | ⨷ | ⨴ | ⨴ |
Run 10 | 100 | 10−4 | 1021 | 25.6 | 3.1 | 6.4 | ⨴ | ⨷ | ⨷ | ⨷ | ⨷ | ⨷ |
Run 11 | 150 | 10−4 | 1021 | 18.3 | 1.8 | 3.9 | ⨴ | ⨵ | ⨵ | ⨵ | ⨵ | |
