Imaging of post‐collisional deformations on the <scp>NE</scp> Tisza continental unit using ambient seismic noise: A case study from the Țicău area, Romania

The Ţicău area (NW Romania) is part of the collisional zone between Tisza and Dacia mega-units. Imaging area's subsurface geological structure will contribute to understanding processes, which controlled its tectonic evolution. Analysis outcrops provides accurate information for building kinematic sections used explain small-scale deformations sedimentary formations, such as those developed south mountains. large-scale requires analysis data recorded and/or measured over a wider area. We use Seismic Interferometry by cross-correlation on ambient noise along with line located north passive seismic section obtained after virtual body-wave reflections processing displays folded faulted Paleogene are in good agreement observations found active-source same too noisy interpretation.