The pressure-temperature (P–T) paths for the ultrahigh-pressure (UHP) metamorphic units in the Western Alps (IMAGE)
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The P–T path for the Sesia zone (continental origin) is from the present study. The P-T paths obtained by previous studies for the Lago di Cignana Unit (oceanic origin) from the Piemont-Liguria Zone and Brossasco-Isasca Unit (continental origin) from the Dora-Maira Massif are shown for comparison.
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