Reply to: Discussion on «Geological map of the partially dolomitized Jurassic succession exposed in the central sector of the Montagna dei Fiori Anticline, Central Apennines, Italy» by M. Santantonio, S. Fabbi & S. Bigi

We welcome the discussion of our paper on the geological map of the central sector of the Montagna dei Fiori by Santantonio and co-workers, because this will contribute to improving the understanding of the complex geological setting of the area and, eventually, helping to disentangle the pre-orogenic and syn-orogenic evolutionary history that is recorded in the tectono-sedimentary pattern exposed in the Montagna dei Fiori anticline.