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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Leisureliness

Sputum

提升

Environmental Controls and Facies Architecture of a Jurassic Carbonate Episode (La Manga Formation),-3) represented by transgressive and highstand systems tracts with sequence boundaries of regional character. Different controlling factors can be recognised in the deposition of this unit. The abrupt changes of facies, as well as paleokarst and epikarst discontinuity surfaces in the successions pro

不安

Substitution

gentle

Tectonic Setting of the Tordillo Formation in the Aconcagua Fold-and-Thrust Beltas located to the E-SE, and that the underlying units were exhumed at the time of deposition of the Late Jurassic red beds. A consistent thickness increment of the Upper Jurassic deposits to the west through the Aconcagua fold-and-thrust belt suggests that sedimentation was controlled by NNW-directe

microscopic

Magnetostratigraphy of the Jurassic Through Lower Cretaceous in the Neuquén Basinrse (Jr1–Jr16) and 16 normal (Jn1–Jn16) polarity zones that encompass at least 19 ammonite zones. A major difference between both scales rises in the Hettangian involving the Jr1–Jr3 polarity zones. For the Middle Jurassic, the resultant magnetostratigraphy obtained in the Lajas Formation outlines a

prostate-gland

Orbital Controls and High-Resolution Cyclostratigraphy of Late Jurassic–Early Cretaceous in the Neuqtratigraphy enabled the construction of almost continuous floating astronomical time scale for the Tithonian–Hauterivian, for which a minimum duration of 5.67 myr for the Tithonian, 5.27 myr for the Berriasian, >3.45 myr for the Valanginian, and 5.96 myr for the Hauterivian have been assessed. Addit

Narrative