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High- and ultrahigh-pressure metamorphic crustal rocks in orogenic belts provide evidence for subduction into the mantle and subsequent exhumation. The timing of metamorphism(s) of complex high- and ultrahigh-pressure rocks can be registered in the robust mineral zircon, able to preserve different growth generations. Here we present sensitive high resolution ion microprobe (SHRIMP) U–Pb age and REE...
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