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Titlebook: Opening and Closure of the Neuquén Basin in the Southern Andes; Diego Kietzmann,Andrés Folguera Book 2020 Springer Nature Switzerland AG 2

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Thermochronological Constraints on the Exhumation of the Malargüe Fold-Thrust Belt, Southern Central cooling in hinterland sectors of the MFTB coupled with thin-skinned shortening and retroarc foreland basin development to the east. By 10–7 Ma, continued shortening reactivated the easternmost frontal structures (e.g., Río Atuel fault) and partially inverted the Neuquén Basin. Subsequent deformatio
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Late Cretaceous to Oligocene Magmatic Evolution of the Neuquén Basinth American plate with higher convergence rates. Then extensional basins and associated magmatism developed at this time destabilizing the Paleogene fold and thrust belt and establishing a more homogeneous tholeiitic signature along the Andean axis.
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2197-9596 nd 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..978-3-030-29682-7978-3-030-29680-3Series ISSN 2197-9596 Series E-ISSN 2197-960X
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Opening and Closure of the Neuquén Basin in the Southern Andes
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