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Are there any 3.8 Ga rock at Anshan in the North China Craton? Reply to comments on Zircon U-Pb and Hf isotopic constraints on the Early Archean crustal evolution in Anshan of the North China Craton by Nutman et al. Reply
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Integrated field geological and zircon morphology evidence for ca. 3.8 Ga rocks at Anshan: Comment on Zircon U-Pb and Hf isotopic constraints on the Early Archean crustal evolution in Anshan of the North China Craton by Wu et al. [Precambrian Res. 167 (2008) 339-362]
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U-Pb ages (3.8-2.7 Ga) and Nd isotope data from the newly identified Eoarchean Nuvvuagittuq supracrustal belt, Superior Craton, Canada
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Early (≥ 4.5 Ga) formation of terrestrial crust:: Lu-Hf, δ18O, and Ti thermometry results for Hadean zircons
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Geochemical fingerprinting of oceanic basalts with applications to ophiolite classification and the search for Archean oceanic crust
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Zircon U-Pb and Hf isotopic constraints on the Early Archean crustal evolution in Anshan of the North China Craton
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Alteration and geochemical patterns in the 3.7-3.8 Ga Isua greenstone belt, West Greenland
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