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

Citation

Taylor, J, Stevens, G, Armstrong, R et al 2010, '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', Precambrian Research, vol. 177, no. 1-2, pp. 88-102.

Year

2010

ANU Authors

Fields of Research

  • Igneous And Metamorphic Petrology
  • Geochronology
  • Tectonics

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