LEADER 03518nam 22005535 450 001 9910337910003321 005 20200630011046.0 010 $a3-030-11190-3 024 7 $a10.1007/978-3-030-11190-8 035 $a(CKB)4100000008339100 035 $a(MiAaPQ)EBC5780765 035 $a(DE-He213)978-3-030-11190-8 035 $a(PPN)236523589 035 $a(EXLCZ)994100000008339100 100 $a20190528d2019 u| 0 101 0 $aeng 135 $aurcnu|||||||| 181 $ctxt$2rdacontent 182 $cc$2rdamedia 183 $acr$2rdacarrier 200 14$aThe Geology of Iberia: A Geodynamic Approach $eVolume 4: Cenozoic Basins /$fedited by Cecilio Quesada, José Tomás Oliveira 205 $a1st ed. 2019. 210 1$aCham :$cSpringer International Publishing :$cImprint: Springer,$d2019. 215 $a1 online resource (195 pages) 225 1 $aRegional Geology Reviews,$x2364-6438 311 $a3-030-11189-X 327 $a1. Preface -- 2. Cenozoic basins in Iberia: an introduction -- 3.Alpine foreland basins -- 4.Extension in the West Mediterranean -- 5.Cenozoic basins of western Iberia (Mondego, Lower Tejo and Alvalade basins) -- 6. Late-orogenic intermontane foreland basins in Iberia -- 7. Cenozoic magmatism in Iberia. 330 $aPursuing an innovative, global approach, this unique book provides an updated review of the geology of Iberia and its continental margins from a geodynamic perspective. Owing to its location close to successive plate margins, Iberia has played a pivotal role in the geodynamic evolution of the Gondwanan, Rheic, Pangea, Tethys and Eurasian plates over the last 600 Ma of Earth?s history. The geological record starts with the amalgamation of Gondwana in the Neoproterozoic, which was succeeded by the rifting and spreading of the Rheic ocean; its demise, which led to the amalgamation of Pangea in the late Paleozoic; the rifting and spreading of several arms of the Neotethys ocean in the Mesozoic Era and their ongoing closure, which was responsible for the Alpine orogeny. The significant advances in the last 20 years have increasingly attracted international interest in exploring the geology of the Iberian Peninsula. This volume focuses on the Cenozoic basins of the Iberian Geology and consequently the most recent sedimentary features in the Iberian Geology apart of the active ones. In this book, you will find a detailed explanation of the alpine foreland basins, the extension of the west Mediterranean as well as the latest magmatism in Iberia. 410 0$aRegional Geology Reviews,$x2364-6438 606 $aGeology 606 $aGeophysics 606 $aNatural disasters 606 $aGeology$3https://scigraph.springernature.com/ontologies/product-market-codes/G17002 606 $aGeophysics/Geodesy$3https://scigraph.springernature.com/ontologies/product-market-codes/G18009 606 $aNatural Hazards$3https://scigraph.springernature.com/ontologies/product-market-codes/G32000 615 0$aGeology. 615 0$aGeophysics. 615 0$aNatural disasters. 615 14$aGeology. 615 24$aGeophysics/Geodesy. 615 24$aNatural Hazards. 676 $a551.78 676 $a554.46 702 $aQuesada$b Cecilio$4edt$4http://id.loc.gov/vocabulary/relators/edt 702 $aOliveira$b José Tomás$4edt$4http://id.loc.gov/vocabulary/relators/edt 906 $aBOOK 912 $a9910337910003321 996 $aGeology of Iberia: A Geodynamic Approach$92570087 997 $aUNINA