Cenozoic landforms and post-orogenic landscape evolution of the Balkanide orogen: Evidence for alternatives to the tectonic denudation narrative in southern Bulgaria
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文摘

Rock-cooling histories document morphotectonic evolution in the Bulgarian highlands.

Three successive extensional tectonic regimes and associated landforms are documented.

Some rangetop erosion surfaces indicate low rates of geomorphic activity since ~ 45 Ma.

Denudation gradients record the southward migration of subduction trench rollback.

Patterns do not support existing views about supradetachment faulting in the region.

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