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0 Ga. 00 Ga (Rosen and Turkina 2007). 51 Ga. 28 Ga represent metamorphism and contamination. Paleo-pressure and temperature estimates suggest an origin of TTG gneiss under pressures of ∼10 kb. 1 Ga. 85 Ga. 8 Ga. 46 Ga tonalitic gneisses is likely. 0 Ga. The eastern part of the Aldan shield contains Late Archaean and paleo-Proterozoic rocks. 8 Ga components: (1) Baijiafen mylonitized trondhjemitic rocks; (2) Dongshan banded trondhjemitic rocks, and (3) Dongshan meta-quartz diorite (Song et al. 1996; Liu et al.

2003). Chamberlain and Mueller interpreted the evidence in terms of combination of erosion of early Archaean cratons and subduction of basaltic crust including cratonderived sediments into the mantle. 85 Ga was associated with multiple intrusions of tonalitetrondhjemite-granodiorite and K-granites in the Beartooth-Bighorn Magmatic Zone, forming broad plutonic blooms rather than arc trench-type linear belts (Frost et al. 2006; Mueller and Frost 2006). 63 Ga in the southern part of the craton. 3 Ga craton is provided by a, at least 100,000 km2 large, 15–25 km thick and seismically-fast lower crustal layer imaged beneath the Bighorn subprovince by the Deep Probe experiment (Nelson 1999; Gorman et al.

66 Ga, which is coincident with the protolith age of an adjacent tonalitic gneiss. Scale bars are 50 μm. Values record 207Pb/206Pb ages (2σ). “D” and “T” represent analytical spots of LA-ICPMS dating and LA-ICPMS trace element analysis, respectively (Iizuka et al. 2007; Elsevier, by permission) (Hodges et al. 1995; Sano et al. 26 Ga MacKenzie mafic dyking event (LeCheminant and Heaman 1989; Bleeker and Stern 1997). 8 Ga, is composed of Archaean plutonic suites containing 1–10 km-wide belts of amphibolite and granulite-facies greenstones traced up to 150 km along strike (Percival and Card 1994; Percival et al.

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