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

[1]  Dunyi Liu,et al.  High-temperature metamorphism and crustal melting at ca. 3.2 Ga in the eastern Kaapvaal craton, southern Africa , 2018, Precambrian Research.

[2]  G. Stevens,et al.  Zircon geochronology and Hf isotopes of the Dwalile Supracrustal Suite, Ancient Gneiss Complex, Swaziland: Insights into the diversity of Palaeoarchaean source rocks, depositional and metamorphic ages , 2017 .

[3]  A. Gerdes,et al.  U–Pb–Hf isotope systematics of detrital zircons in high-grade paragneisses of the Ancient Gneiss Complex, Swaziland: Evidence for two periods of juvenile crust formation, Paleo- and Mesoarchaean sediment deposition, and 3.23 Ga terrane accretion , 2016 .

[4]  G. Nicoli,et al.  Diversity of burial rates in convergent settings decreased as Earth aged , 2016, Scientific Reports.

[5]  A. Hofmann,et al.  Source composition, fractional crystallization and magma mixing processes in the 3.48–3.43 Ga Tsawela tonalite suite (Ancient Gneiss Complex, Swaziland) – Implications for Palaeoarchaean geodynamics , 2016 .

[6]  G. Stevens,et al.  Reply to “Paleo- to Mesoarchean polymetamorphism in the Barberton granite-greenstone belt, South Africa: Constraints from U-Pb monazite and Lu-Hf garnet geochronology on the tectonic processes that shaped the belt: Discussion” by M. Brown , 2015 .

[7]  Dunyi Liu,et al.  Generation of early Archaean grey gneisses through melting of older crust in the eastern Kaapvaal craton, southern Africa , 2014 .

[8]  J. Hoffmann,et al.  Archaean granulite-facies paragneisses from central Swaziland: inferences on Palaeoarchaean crustal reworking and a complex metamorphic history , 2014, Journal of the Geological Society.

[9]  M. V. Kranendonk,et al.  Just another drip: Re-analysis of a proposed Mesoarchean suture from the Barberton Mountain Land, South Africa , 2014 .

[10]  I. Buick,et al.  Paleo- to Mesoarchean polymetamorphism in the Barberton Granite-Greenstone Belt, South Africa: Constraints from U-Pb monazite and Lu-Hf garnet geochronology on the tectonic processes that shaped the belt , 2014 .

[11]  J. Moyen,et al.  Experimental Constraints on TTG Petrogenesis: Implications for Archean Geodynamics , 2013 .

[12]  Peter A. Cawood,et al.  Detrital zircon record and tectonic setting , 2012 .

[13]  I. Buick,et al.  Successive midcrustal, high-grade metamorphic events provide insight into Mid-Archean mountain-building along the SE margin of the proto-Kaapvaal craton , 2012 .

[14]  M. V. Van Kranendonk.  Onset of Plate Tectonics , 2011, Science.

[15]  A. Gerdes,et al.  Hafnium isotope record of the Ancient Gneiss Complex, Swaziland, southern Africa: evidence for Archaean crust–mantle formation and crust reworking between 3.66 and 2.73 Ga , 2011, Journal of the Geological Society.

[16]  A. Kisters,et al.  Continental growth and convergence-related arc plutonism in the Mesoarchaean: Evidence from the Barberton granitoid-greenstone terrain, South Africa , 2010 .

[17]  S. Bowring,et al.  Rates and mechanisms of Mesoarchean magmatic arc construction, eastern Kaapvaal craton, Swaziland , 2010 .

[18]  J. Moyen.  High Sr/Y and La/Yb ratios: The meaning of the “adakitic signature” , 2009 .

[19]  S. Bowring,et al.  Sm–Nd isotopic mapping of lithospheric growth and stabilization in the eastern Kaapvaal craton , 2009 .

[20]  J. Moyen,et al.  Record of mid-Archaean subduction from metamorphism in the Barberton terrain, South Africa , 2006, Nature.

[21]  J. Diener,et al.  Metamorphism and exhumation of the basal parts of the Barberton greenstone belt, South Africa: Constraining the rates of Mesoarchaean tectonism , 2005 .

[22]  G. Stevens,et al.  Extensional detachment faulting and core-complex formation in the southern Barberton granite–greenstone terrain, South Africa: evidence for a 3.2 Ga orogenic collapse , 2003 .

[23]  A. Kröner,et al.  Gneiss-greenstone relationships in the Ancient Gneiss Complex of southwestern Swaziland, southern Africa, and implications for early crustal evolution , 1994 .