Ocean basins are created along blank convergent boundaries that break apart continental lithosphere.
Converging boundaries produce foreland basins through tectonic compression of oceanic and continental crust during lithospheric flexure. The collapse of the rift zone or the emergence of an ocean might result from tectonic extension at divergent borders when continental rifting is taking place.
The North Sea is an illustration of a basin created by lithospheric stretching; it is also a prominent site for considerable hydrocarbon deposits. Another comparable feature is the Basin and Range province, which forms a sequence of horst and graben formations and occupies the majority of the US state of Nevada.
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