Statistics for Granulite facies anatexis in the Ancient Gneiss Complex, Swaziland, at 2.73 Ga: Mid-crustal metamorphic evidence for mantle heating of the Kaapvaal craton during Ventersdorp magmatism
Total visits
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| Granulite facies anatexis in the Ancient Gneiss Complex, Swaziland, at 2.73 Ga: Mid-crustal metamorphic evidence for mantle heating of the Kaapvaal craton during Ventersdorp magmatism | 4 |
Total visits per month
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| April 2024 | 0 |
| May 2024 | 0 |
| June 2024 | 0 |
| July 2024 | 0 |
| August 2024 | 3 |
| September 2024 | 0 |
| October 2024 | 0 |