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Opening and closure of the Neuquen B...

Folguera, Andres.

Opening and closure of the Neuquen Basin in the Southern Andes

Record Type:	Electronic resources : Monograph/item
Title/Author:	Opening and closure of the Neuquen Basin in the Southern Andesedited by Diego Kietzmann, Andres Folguera.
other author:	Kietzmann, Diego.
Published:	Cham :Springer International Publishing :2020.
Description:	xx, 513 p. :ill. (some col.), digital ;24 cm.
Contained By:	Springer eBooks
Subject:	Basins (Geology)Argentina
Online resource:	https://doi.org/10.1007/978-3-030-29680-3
ISBN:	9783030296803$q(electronic bk.)

Opening and closure of the Neuquen Basin in the Southern Andes
Opening and closure of the Neuquen Basin in the Southern Andes[electronic resource] /edited by Diego Kietzmann, Andres Folguera. - Cham :Springer International Publishing :2020. - xx, 513 p. :ill. (some col.), digital ;24 cm. - Springer earth system sciences,2197-9596. - Springer earth system sciences..

The Neuquen 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 Neuquen Basin -- Orbital controls and high-resolution cyclostratigraphy of Late Jurassic - Early Cretaceous in the Neuquen Basin (Lower Callovian - Early Barremian) -- Sedimentary evolution of the continental Late Cretaceous Neuquen Group -- The Cretaceous contractional stage and the first synorogenic basin in the Neuquen Basin -- The origin of the Malargue 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 Malargue fold and thrust belt -- The structure of the Malargue fold and thrust belt -- Thermochronological constraints on the exhumation of the Malargue 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 Neuquen Basin and the impact of the Payenia hot spot.

This book provides an overview of newly gathered material focusing on the opening and closure of The Neuquen Basin. The Neuquen 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.

ISBN: 9783030296803$q(electronic bk.)

Standard No.: 10.1007/978-3-030-29680-3doiSubjects--Topical Terms:

860795
Basins (Geology)
--Argentina

LC Class. No.: QE231 / .O646 2020

Dewey Class. No.: 551.44

Opening and closure of the Neuquen Basin in the Southern Andes
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505 0 $a The Neuquen 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 Neuquen Basin -- Orbital controls and high-resolution cyclostratigraphy of Late Jurassic - Early Cretaceous in the Neuquen Basin (Lower Callovian - Early Barremian) -- Sedimentary evolution of the continental Late Cretaceous Neuquen Group -- The Cretaceous contractional stage and the first synorogenic basin in the Neuquen Basin -- The origin of the Malargue 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 Malargue fold and thrust belt -- The structure of the Malargue fold and thrust belt -- Thermochronological constraints on the exhumation of the Malargue 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 Neuquen Basin and the impact of the Payenia hot spot.
520 $a This book provides an overview of newly gathered material focusing on the opening and closure of The Neuquen Basin. The Neuquen 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.
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