LEADER 05520nam 22006855 450 001 9910373887103321 005 20200704054236.0 010 $a3-030-29680-6 024 7 $a10.1007/978-3-030-29680-3 035 $a(CKB)4900000000505183 035 $a(DE-He213)978-3-030-29680-3 035 $a(MiAaPQ)EBC6026458 035 $a(PPN)242846521 035 $a(EXLCZ)994900000000505183 100 $a20200114d2020 u| 0 101 0 $aeng 135 $aurnn|008mamaa 181 $ctxt$2rdacontent 182 $cc$2rdamedia 183 $acr$2rdacarrier 200 10$aOpening and Closure of the Neuquén Basin in the Southern Andes /$fedited by Diego Kietzmann, Andrés Folguera 205 $a1st ed. 2020. 210 1$aCham :$cSpringer International Publishing :$cImprint: Springer,$d2020. 215 $a1 online resource (XX, 513 p. 177 illus., 165 illus. in color.) 225 1 $aSpringer Earth System Sciences,$x2197-9596 311 $a3-030-29679-2 320 $aIncludes bibliographical references. 327 $aThe Neuquén Basin: Stratigraphy, subsidence controls and basin closure -- Heterogeneities and syn-rift evolution of Late Triassic-Early Jurassic Precuyano Cycle -- Structure of the Precuyo synrift in the Valenciana depocenter -- Structure of the Precuyo synrift in the Cara Cura-Sierra de Reyes depocenter -- Early Jurassic magmatism -- High-resolution sequence stratigraphy and main controls of the Middle Jurassic Cuyo Group -- Depositional environments and hyperpycnal shelfal sedimentation in the Late Jurassic Lotena Formation -- Environmental controls and facies architecture of a Late Jurassic (Oxfordian) carbonate episode (La Manga Formation) -- The Cuyo and lower Mendoza cycles in the Aconcagua fold and thrust belt -- The extensional control of the Late Jurassic units -- Morphostructural configuration and sedimentary evolution of the Late Jurassic ? Early Cretaceous Vaca Muerta ?Quintuco system -- Magnetostratigraphy of the Early Jurassic ? Early Cretaceous in the Neuquén Basin -- Orbital controls and high-resolution cyclostratigraphy of Late Jurassic ? Early Cretaceous in the Neuquén Basin (Lower Callovian ? Early Barremian) -- Sedimentary evolution of the continental Late Cretaceous Neuquén Group -- The Cretaceous contractional stage and the first synorogenic basin in the Neuquén Basin -- The origin of the Malargüe Basin -- The Late Cretaceous-Paleocene extension -- The Paleocene to early Oligocene lull -- Causes and extent of the Oligocene extension -- The Late Cretaceous to Oligocene magmatism -- The Miocene orogenesis related to the subduction of the Payenia hot spot -- The Miocene magmatism in the Malargüe fold and thrust belt -- The structure of the Malargüe fold and thrust belt -- Thermochronological constraints on the exhumation of the Malargüe fold and thrust belt -- Structure and thermochronological constraints on the exhumation of the Chos Malal fold and thrust belt -- The structure and exhumation of the Agrio fold and thrust belt -- The Quaternary deformation in the Neuquén Basin and the impact of the Payenia hot spot. 330 $aThis book provides an overview of newly gathered material focusing on the opening and closure of The Neuquén Basin. The Neuquén Basin contains the most important hydrocarbon reservoirs in Argentina and therefore is characterized by a profound knowledge of the sedimentation mechanisms and closure times. During the last 10 years a considerable amount of new information has been produced that illustrates a complex evolution that involves more than one synrift stage during its evolution, an aborted sag phase associated with the inception of a first foreland basin in late Early Cretaceous times, two extensional destabilizations in the Late Cretaceous-Paleocene and late Oligocene times and a Neogene magmatic expansion coetaneous to a last mountain building. These processes have produced a polyphasic complex structure that exhumed the rich sedimentary record that characterizes the basin. 410 0$aSpringer Earth System Sciences,$x2197-9596 606 $aPhysical geography 606 $aHydrology 606 $aHydrogeology 606 $aPaleoecology 606 $aSedimentology 606 $aPhysical Geography$3https://scigraph.springernature.com/ontologies/product-market-codes/J16000 606 $aHydrology/Water Resources$3https://scigraph.springernature.com/ontologies/product-market-codes/211000 606 $aHydrogeology$3https://scigraph.springernature.com/ontologies/product-market-codes/G19005 606 $aPaleoecology$3https://scigraph.springernature.com/ontologies/product-market-codes/U21010 606 $aSedimentology$3https://scigraph.springernature.com/ontologies/product-market-codes/G17080 615 0$aPhysical geography. 615 0$aHydrology. 615 0$aHydrogeology. 615 0$aPaleoecology. 615 0$aSedimentology. 615 14$aPhysical Geography. 615 24$aHydrology/Water Resources. 615 24$aHydrogeology. 615 24$aPaleoecology. 615 24$aSedimentology. 676 $a551.44 702 $aKietzmann$b Diego$4edt$4http://id.loc.gov/vocabulary/relators/edt 702 $aFolguera$b Andrés$4edt$4http://id.loc.gov/vocabulary/relators/edt 801 0$bMiAaPQ 801 1$bMiAaPQ 801 2$bMiAaPQ 906 $aBOOK 912 $a9910373887103321 996 $aOpening and Closure of the Neuquén Basin in the Southern Andes$92017443 997 $aUNINA