Episodic growth of the Gondwana supercontinent from hafnium and oxygen isotopes in zircon

By AJ Kemp, C. Hawkesworth, B. Paterson, P. Kinny. Nature, 2006

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View Paper: https://www.semanticscholar.org/paper/8b1f49d54712b31b57a570d373b0556632739a4d

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In Geophysics

Citations in the corpus

Hafnium isotope characterization of the GJ-1 zircon reference material by solution and laser-ablation MC-ICPMS (2008, background): “, 2005; Hawkesworth and Kemp, 2006), in provenance studies of sediments (e.g., Griffin et al., 2004; Condie et al., 2005; Griffin et al., 2006a; Kemp et al., 2006), and into magmatic processes (Kemp et al.”
Rutile crystals as potential trace element and isotope mineral standards for microanalysis (2009, background): “Very low Lu concentrations (see Table 3) obtained for all grains are evidence for no radiogenic ingrowth, making rutile particularly useful for calculating Hf isotope composition of source rocks (e.g., Griffin et al., 2004; Choukroun et al., 2005; Hawkesworth and Kemp, 2006; Kemp et al., 2006).”
Partial melting of lower crust at 10–15 kbar: constraints on adakite and TTG formation (2013, background): “Recent hafnium and oxygen isotopes coupled with precise zircon U–Pb dating demonstrate that some of the TTG rocks represent crust reworking through anatexis of pre-existing mafic lower crust (Whalen et al. 2002; Kemp et al. 2006; Jahn et al. 2008; Jiang et al. 2010; Rollinson 2012).”
Multiscale magmatic cyclicity, duration of pluton construction, and the paradoxical relationship between tectonism and plutonism in continental arcs (2011, background): “Additionally, important questions were raised about the entire system at the crustal scale, particularly themechanisms and rate of crustal growth (Ducea, 2001; Kemp et al., 2006; Hawkesworth and Kemp, 2006; Kemp et al., 2007; DeCelles et al., 2009).”