The Black Sea consists of two oceanic basins separated by the mid-Blac
k Sea ridge. The east-west-oriented west Black Sea basin opened as a b
ack-arc rift in the Cretaceous by tearing a Hercynian continental sliv
er, the Istanbul zone, from the present-day Odessa shelf. The Istanbul
zone, which was initially contiguous with the Moesian platform in the
west, moved south during the Late Cretaceous-Paleocene with respect t
o the Odessa shelf along two transform faults: the dextral west Black
Sea and the sinistral west Crimean faults. It collided in the early Eo
cene with a Cimmeride zone in the south, thereby ending the extension
in the western Black Sea and deactivating both the west Black Sea and
the west Crimean faults as strike-slip faults. The east Black Sea basi
n opened as a result of the counterclockwise rotation of an east Black
Sea block around a rotation pole located north of the Crimea. This bl
ock was bounded by the west Crimean fault, the southern margin of the
eastern Black Sea, and the southern frontal thrusts of the Greater Cau
casus. The rotation of the east Black Sea block was contemporaneous wi
th the rifting of the west Black Sea basin but lasted until the Miocen
e, resulting in continuous compression along the Greater Caucasus.