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Such a transition is observed in the Black Sea, where the accurate quantification of shortening effects is hampered by the kinematically unclear geometries of Cenozoic inversion. By means of seismic profiles interpretation, quantified deformation features and associated syn\u2010tectonic geometries on the Romanian offshore, this study demonstrates that uplifted areas, observed by exploration studies, form a coherent thick\u2010skinned thrust system with N\u2010ward vergence. Thrusting inverted an existing geometry made up by successive grabens that were inherited from the Cretaceous extensional evolution. The shortening started during late Eocene times and gradually affected all areas of the Western Black Sea Basin during Oligocene and Miocene times, deformation being coherently correlated across its western margin. The mechanism of this generalized inversion is the transmission of stresses during the collision recorded in the Pontides\u2010Balkanides system. Syn\u2010tectonic sedimentation in the Western Black Sea demonstrates that this process was continuous and took place through the onset of gradual shortening migrating northward. Although the total amount of shortening is roughly constant in an E\u2010W direction, individual thrusts have variable offsets, deformation being transferred between structures located at distance across the strike of the system. The Black Sea example demonstrates that the vergence and offset of thrusts can change rapidly along the strike of such a compressional back\u2010arc system. This generates apparently contrasting geometries that accommodate the same orogenic shortening.<\/jats:p>","DOI":"10.1029\/2011tc002865","type":"journal-article","created":{"date-parts":[[2011,8,5]],"date-time":"2011-08-05T14:52:54Z","timestamp":1312555974000},"source":"Crossref","is-referenced-by-count":64,"title":["Kinematics of back\u2010arc inversion of the Western Black Sea Basin"],"prefix":"10.1029","volume":"30","author":[{"given":"I.","family":"Munteanu","sequence":"first","affiliation":[{"name":"Faculty of Geology and Geophysics University of Bucharest  Bucharest Romania"},{"name":"Netherlands Research Centre for Integrated Solid Earth Science VU University Amsterdam  Amsterdam Netherlands"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"L.","family":"Matenco","sequence":"additional","affiliation":[{"name":"Netherlands Research Centre for Integrated Solid Earth Science VU University Amsterdam  Amsterdam Netherlands"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"C.","family":"Dinu","sequence":"additional","affiliation":[{"name":"Faculty of Geology and Geophysics University of Bucharest  Bucharest Romania"},{"name":"Netherlands Research Centre for Integrated Solid Earth Science VU University Amsterdam  Amsterdam Netherlands"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"S.","family":"Cloetingh","sequence":"additional","affiliation":[{"name":"Netherlands Research Centre for Integrated Solid Earth Science VU University Amsterdam  Amsterdam Netherlands"}],"role":[{"vocabulary":"crossref","role":"author"}]}],"member":"13","published-online":{"date-parts":[[2011,9,17]]},"reference":[{"key":"e_1_2_7_2_1","doi-asserted-by":"publisher","DOI":"10.1016\/0040\u20101951(77)90065\u20108"},{"key":"e_1_2_7_3_1","volume-title":"Geology of the Eastern Black Sea","author":"Afanasenkov A. 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