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"otype" : "Journal", "mtid" : 1722, "link" : "/api/journal/1722", "label" : "GLOBAL AND PLANETARY CHANGE 0921-8181 1872-6364", "pIssn" : "0921-8181", "eIssn" : "1872-6364", "reviewType" : "REVIEWED", "noIF" : false, "sciIndexed" : true, "scopusIndexed" : true, "lang" : "FOREIGN", "hungarian" : false, "published" : true, "oldId" : 1722, "snippet" : true }, "volume" : "58", "issue" : "1-4", "firstPage" : "165", "lastPage" : "180", "firstPageOrInternalIdForSort" : "165", "pageLength" : 16, "publishedYear" : 2007, "abstractText" : "This paper presents a latest compilation of data on the present-day\nstress pattern in the Pannonian basin, and its tectonic environment,\nthe Alpine-Dinaric orogens. Extensional formation of the basin system\ncommenced in the early Miocene, whereas its structural reactivation, in\nthe form of gradual basin inversion, has been taking place since\nPliocene to recent times. Reconstructed compression and associated\nhorizontal contraction are mainly governed by the convergence between\nAdria and its buffer, the Alpine belt of orogens. The resulting\ncontemporaneous stress field exhibits important lateral variation\nresulting in a complex pattern of ongoing tectonic activity. In the\nFriuli zone of the Southern Alps, where thrust faulting prevails,\ncompression is orthogonal to the strike of the mountain belt. More to\nthe southeast, intense contraction is combined with active strike-slip\nfaulting constituting the dextral Dinaric transpressional corridor.\nStresses are transferred far from Adria into the Pannonian basin, and\nthe dominant style of deformation gradually changes from pure\ncontraction through transpression to strike-slip faulting. The\nimportance of late-stage inversion in the Pannonian basin is\ninterpreted in a more general context of structural reactivation of\nbackarc basins where the sources of compression driving basin inversion\nare also identified and discussed. The state of recent stress and\ndeformation in the Pannonian basin, particularly in its western and\nsouthern part, is governed by the complex interaction of plate boundary\nand intra-plate forces. The counterclockwise rotation and\nnorth-northeast-directed indentation of the Adriatic microplate appears\nto be of key importance as the dominant source of compression\n(\"Adria-push\"). Intra-plate stress sources, such as buoyancy forces\nassociated with an elevated topography, and crustal as well as\nlithospheric inhomogeneities can also play essential, yet rather local\nrole. (C) 2007 Elsevier B.V. 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