Kinematics of back-arc inversion of the Western Black Sea Basin

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Kinematics of back‐arc inversion of the Western Black Sea Basin

[1] Back‐arc basin evolution is driven by processes active at the main subduction zone typically assuming the transition from an extensional back‐arc, during the retreat of a mature slab, to a contractional basin, during high‐strain collisional processes. Such a transition is observed in the Black Sea, where the accurate quantification of shortening effects is hampered by the kinematically uncl...

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ژورنال

عنوان ژورنال: Tectonics

سال: 2011

ISSN: 0278-7407

DOI: 10.1029/2011tc002865