Multiple metamorphic stages within an eclogite-facies terrane (Sesia Zone, Western Alps) revealed by Th-U-Pb petrochronology
Convergent plate margins typically experience a transition from subduction to collision dynamics as massive continental blocks enter the subduction channel. Studies of high-pressure rocks indicate that tectonic fragments are rapidly exhumed from eclogite
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|Source:||Journal of Petrology|
|01_Regis_Multiple_metamorphic_stages_2014.pdf||5.26 MB||Adobe PDF||Request a copy|
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