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010   $a3-030-10519-9
024 7 $a10.1007/978-3-030-10519-8
035   $a(CKB)4100000009046505
035   $a(MiAaPQ)EBC5855442
035   $a(DE-He213)978-3-030-10519-8
035   $a(PPN)248602764
035   $a(EXLCZ)994100000009046505
100   $a20190820d2019      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 $eVolume 2: The Variscan Cycle /$fedited by Cecilio Quesada, José Tomás Oliveira
205   $a1st ed. 2019.
210  1$aCham :$cSpringer International Publishing :$cImprint: Springer,$d2019.
215   $a1 online resource (560 pages) $cillustrations
225 1 $aRegional Geology Reviews,$x2364-6446
311 08$a3-030-10518-0 
320   $aIncludes bibliographical references.
327   $a1. Introduction -- 2.Precambrian Basement -- 3.Variscan Cycle -- 4.Alpine Cycle -- 5. Cenozoic Basins -- 6. Lithospheric Structure of Iberia, the Balearic Islands and the Continental Shelves -- 7.Relief and Active Processes.
330   $aTaking a new global approach, this unique book provides an updated review of the geology of Iberia and its continental margins from a geodynamic perspective. Owing to its location close to successive plate margins, Iberia has played a pivotal role in the geodynamic evolution of the Gondwanan, Rheic, Pangea, Tethys s.l. and Eurasian plates over the last 600 Ma of Earth's history. The geological record starts with the amalgamation of Gondwana in the Neoproterozoic succeeded by the rifting and spreading of the Rheic ocean; its demise, which led to the amalgamation of Pangea in the late Paleozoic; the rifting and spreading of several arms of the Neotethys ocean in the Mesozoic Era and their ongoing closure, which was responsible for the Alpine orogeny. The significant advances in the last 20 years have attracted international research interest in the geology of the Iberian Peninsula. This volume presents the most comprehensive, careful and updated description of the variscan cycle in Iberia. This volume focuses in the different geological events since the Cambrian-Early Ordovician rift until the late variscan orocline formations including magmatic and metamorphic evolution.
410  0$aRegional Geology Reviews,$x2364-6446
606   $aGeology
606   $aGeophysics
606   $aMineralogy
606   $aPaleontology
606   $aGeology
606   $aGeophysics
606   $aMineralogy
606   $aPaleontology
615  0$aGeology.
615  0$aGeophysics.
615  0$aMineralogy.
615  0$aPaleontology.
615 14$aGeology.
615 24$aGeophysics.
615 24$aMineralogy.
615 24$aPaleontology.
676   $a550
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   $a9910341853203321
996   $aGeology of Iberia$94342597
997   $aUNINA