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The Vrancea seismogenic zone of Romania is a steeply NW-dipping volume (30 × 70 × 200 km) of intermediate-depth seismicity in the upper mantle beneath the bend zone of the Eastern Carpathians. It is widely held that the source of this seismicity is the remnant of a Miocene-age subduction zone. However, recent deep seismic-refl ection data collected over the Eastern Carpathian bend zone image an orogen lacking (1) a crustal root and (2) dipping crustal-scale fabrics routinely imaged in modern and ancient subduction zones. Here, we use these data to evaluate the lithospheric structure of the Eastern Carpathians as it relates to the Vrancea seismogenic zone. Crustal architecture obtained from these data indicate the 140-km-wide orogen is only supported by ~33-km-thick crust, while the adjacent Transylvanian and Focsani basins have ~37-(possibly up to ~46 km) and 42-km-thick crust, respectively. Because the Vrancea seismogenic zone is located beneath the east side of the thin orogenic crust, we infer that the lower orogenic crust was removed through continental delamination and is now represented by the mantle seismicity observed in the Vrancea seismogenic zone. These data and their interpretation suggest an alternate means of generating mantle seismicity in the absence of subduction processes.

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