Statistics for Detrital zircons from a Late Palaeozoic accretionary complex of SW Iberia (Variscan Belt) : history of crustal growth and recycling at the Rheic convergent margin
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| Detrital zircons from a Late Palaeozoic accretionary complex of SW Iberia (Variscan Belt) : history of crustal growth and recycling at the Rheic convergent margin | 189 |
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| 35506.pdf | 263 |
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