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Fig. 1. Examples of crustal growth and recycling models, andestimated maximum contribution of �3900 Ma detrital zir-cons to ancient sediments.
Table 1207Pb/206Pb (�1 �) detrital zircon age data, after filtering according to methods described in texta
Fig. 2. and VM90histograms for zircons analysed from metasediments G93errors depicted at the 1s level) and unfiltered206Pb/238U–207Pb/235U concordia diagrams (analytical 207Pb/206Pb age/54/10.
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