Comment on “High-temperature metamorphism and crustal melting at ca. 3.2 Ga in the eastern Kaapvaal craton, southern Africa” by Kröner et al.– why heating of the Ancient Gneiss Complex by a mantle plume at 3.2 Ga is not a viable tectonic model

J Taylor,G Stevens

doi:10.1016/j.precamres.2019.03.008

Comment on “High-temperature metamorphism and crustal melting at ca. 3.2 Ga in the eastern Kaapvaal craton, southern Africa” by Kröner et al.– why heating of the Ancient Gneiss Complex by a mantle plume at 3.2 Ga is not a viable tectonic model

J Taylor, G Stevens

https://doi.org/10.1016/j.precamres.2019.03.008

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Journal: Precambrian research

Publication Date: Mar 20, 2019

Affiliation: Stellenbosch University

#Ancient Gneiss Complex #Eastern Kaapvaal Craton + Show 8 more

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Abstract

Comment on “High-temperature metamorphism and crustal melting at ca. 3.2 Ga in the eastern Kaapvaal craton, southern Africa” by Kröner et al.– why heating of the Ancient Gneiss Complex by a mantle plume at 3.2 Ga is not a viable tectonic model

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