Retrieving "Syn Orogenic Extension" from the archives
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Paleozoic Blue Schist
Linked via "syn-orogenic extension"
Slab Rollback Acceleration: Rapid seaward migration of the trench due to negative buoyancy of the dense, $\text{Iap-Amph}$-bearing slab segment.
Basement Conjugate Faulting: The introduction of low-viscosity granitic melts generated during the syn-orogenic extension phase immediately following continent-continent contact, effectively "lifting" the deeply buried blueschist block along low-angle extensional faults' [6].
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