LEADER 04172nam 22005655 450 001 9910337903603321 005 20200630023649.0 024 7 $a10.1007/978-3-030-11295-0 035 $a(CKB)4100000008525411 035 $a(DE-He213)978-3-030-11295-0 035 $a(MiAaPQ)EBC5802990 035 $a(PPN)248602772 035 $a(EXLCZ)994100000008525411 100 $a20190628d2019 u| 0 101 0 $aeng 135 $aurnn|008mamaa 181 $ctxt$2rdacontent 182 $cc$2rdamedia 183 $acr$2rdacarrier 200 14$aThe Geology of Iberia: A Geodynamic Approach $eVolume 3: The Alpine Cycle /$fedited by Cecilio Quesada, José Tomás Oliveira 205 $a1st ed. 2019. 210 1$aCham :$cSpringer International Publishing :$cImprint: Springer,$d2019. 215 $a1 online resource (XXVIII, 568 p. 267 illus., 227 illus. in color.) 225 1 $aRegional Geology Reviews,$x2364-6438 311 $a3-030-11295-0 311 $a3-030-11294-2 320 $aIncludes bibliographical references. 327 $a1. An introduction to the Alpine cycle -- 2. The Alpine cycle in Iberia: Microplate units and geodynamic stages -- 3.Permian-Triassic rifting stage -- 4.Late Triassic-Middle Jurassic passive margins -- 5. Late Jurassic-Early Cretaceous rifting -- 6. Late Cretaceous post-rift to convergence in Iberia -- 7.Lithological successions of the Internal Betic and Flysch units -- 8. Alpine orogeny: Deformation and structure in the Northern Iberian margin (Pyrenees s.l.) -- 9. Alpine orogeny: Deformation and structure in the Southern Iberian margin (Betics s.l.) -- 10. Alpine orogeny: Deformation and structure in the West and Southwest Iberia Margins -- 11. Alpine orogeny: Intraplate deformation -- 12. Alpine metamorphism in the Betic Internal Zones -- 13. Mesozoic and Cenozoic magmatism in the Betics. 330 $aTaking a new global approach, this unique book provides an updated review of the geology of Iberia and its continental margins from a geodynamic perspective. Owing to its location close to successive plate margins, Iberia has played a pivotal role in the geodynamic evolution of the Gondwanan, Rheic, Pangea, Tethys s.l. and Eurasian plates over the last 600 Ma of Earth's history. The geological record starts with the amalgamation of Gondwana in the Neoproterozoic succeeded by the rifting and spreading of the Rheic ocean; its demise, which led to the amalgamation of Pangea in the late Paleozoic; the rifting and spreading of several arms of the Neotethys ocean in the Mesozoic Era and their ongoing closure, which was responsible for the Alpine orogeny. The significant advances in the last 20 years have attracted international research interest in the geology of the Iberian Peninsula. This volume presents the most comprehensive, and updated description of the Alpine cycle in Iberia. This volume focuses in the different geological events during the Alpine orogeny as well as the lithological succession . This book is of interest not only for scientists of Portugal and Spain but also for geoscientists searching for analogies for oil and gas as well as tourists visiting the main mountain ridges of Iberia such as the Pyrenees. 410 0$aRegional Geology Reviews,$x2364-6438 606 $aGeology 606 $aGeophysics 606 $aPaleontology  606 $aGeology$3https://scigraph.springernature.com/ontologies/product-market-codes/G17002 606 $aGeophysics/Geodesy$3https://scigraph.springernature.com/ontologies/product-market-codes/G18009 606 $aPaleontology$3https://scigraph.springernature.com/ontologies/product-market-codes/G39000 615 0$aGeology. 615 0$aGeophysics. 615 0$aPaleontology . 615 14$aGeology. 615 24$aGeophysics/Geodesy. 615 24$aPaleontology. 676 $a551 676 $a554.6 702 $aQuesada$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 $a9910337903603321 996 $aGeology of Iberia: A Geodynamic Approach$92570087 997 $aUNINA