Table 1 Results of 40Ar/39Ar groundmass incremental heating experiments for S0230 samples.
From: Superplume mantle tracked isotopically the length of Africa from the Indian Ocean to the Red Sea
Sample information | Plateau | Inverse isochron | |||||||
---|---|---|---|---|---|---|---|---|---|
Experiment | Sample | Age ± 2σ (i) | 39Ar (%) | K/Ca | MSWD | n | N | Age ± 2σ (i) | 40Ar/36 Ar intercept ± 2σ |
a17D17844 | MW14DL3-5 | 6.90 ± 0.02 Ma | 72% | 0.357 | 1.35 | 12 | 24 | 6.90 ± 0.02 Ma | 287.03 ± 7.33 |
bVU107-J3_1 | MW14DL3-5 | 6.94 ± 0.03 Ma | 73% | 0.325 | 1.87 | 8 | 15 | 6.89 ± 0.04 Ma | 316.22 ± 10.88 |
a17D17979 | MW14DL2-3 | 6.91 ± 0.02 Ma | 52% | 0.267 | 3.26 | 7 | 24 | 6.89 ± 0.05 Ma | 315.46 ± 31.97 |
bVU107-J2_1 | MW14DL2-3 | 6.99 ± 0.03 Ma | 63% | 0.326 | 2.07 | 6 | 15 | 6.92 ± 0.06 Ma | 321.16 ± 15.79 |
a17D18018 | MW14DL2-2 | 6.97 ± 0.02 Ma | 57% | 0.173 | 0.40 | 11 | 24 | 6.97 ± 0.03 Ma | 354.12 ± 7.97 |
bVU107-J1_1 | MW14DL2-2 | 7.26 ± 0.12 Ma | 43% | 0.168 | 7.94 | 4 | 15 | 6.87 ± 0.88 Ma | 332.07 ± 74.98 |