Remarks on the Oligo-Miocene extensional episode(s) in InnerDinarides: Towards the tectonic constraints of the origin of intra-montagne basins

The ongoing interest in the complex geology of Dinaric orogen, particular, its immediate, post-orogenic evolution (post-Lutetian), has produced a number tectonic solutions, proposing either extensional stage followed by subsidence, with immense lithospheric thinning resulting regional uplift, or even pure uplift episode(s). unclear Late Oligocene?Miocene forces are often interpreted as interchange crustal-scale driven episodes, presumably affecting formation lacustrine mini-basins, referred to ?intra-montagne basins?. A limited available field-based structural interpretations tend explain Miocene crustal-rooted Despite lacking important subsurface data, such wells-derived thickness and other commonly used for reconstruction eventual subsidence stages, provide several deep models setting. In order better understand timing mechanism behind onset Oligo-Miocene Dinaride ?intra-montagne? episode(s), this study uses information precursory oblique convergent margins, further use combination crustal basin modeling tools that could extract more barely data (subsidence rate, source-to-sink patterns, etc). assessment recently published surface constraints, allowed following discussion evaluating set proposed models.