Print Email Facebook Twitter Geological and structural map of the southeastern Pag Island, Croatia: field constraints on the Cretaceous - Eocene evolution of the Dinarides foreland Title Geological and structural map of the southeastern Pag Island, Croatia: field constraints on the Cretaceous - Eocene evolution of the Dinarides foreland Author Mittempergher, Silvia (University of Milano-Bicocca) Succo, Andrea (University of Parma) Bistacchi, Andrea (University of Milano-Bicocca) Storti, Fabrizio (University of Parma) Bruna, P.B.R. (TU Delft Applied Geology) Meda, Marco (ENI) Date 2019 Abstract The sedimentary succession exposed in the Northern Dalmatia Islands mainly consists of Cretaceous to Neogene shallow water carbonates, folded and imbricated within the External Dinarides thrust belt. During Cretaceous times, carbonate sediments were deposed on a heterogeneous, tectonically-influenced carbonate platform, which was then uplifted and eroded, as evidenced by a regional unconformity embracing the Late Cretaceous and Paleocene. Sedimentation resumed during the Eocene, when the area was part of the foreland basin of the Dinaric belt. With our geological and structural map of the southeastern Pag Island at the 1:25,000 scale, we refined the stratigraphic and structural setting and the tectono- sedimentary evolution of the area. Subject Adriatic Carbonate PlatformExternal DinaridesForeland basinPag IslandThrust and fold belt To reference this document use: http://resolver.tudelft.nl/uuid:08b2d508-6113-491b-9a82-5d0be30d9f57 DOI https://doi.org/10.3301/GFT.2019.06 ISSN 2038-4947 Source Geological Field Trips and Maps, 11 (2.4), 2-19 Part of collection Institutional Repository Document type review Rights © 2019 Silvia Mittempergher, Andrea Succo, Andrea Bistacchi, Fabrizio Storti, P.B.R. Bruna, Marco Meda Files PDF GFT2019_11_2_4.pdf 5.45 MB Close viewer /islandora/object/uuid:08b2d508-6113-491b-9a82-5d0be30d9f57/datastream/OBJ/view