Oblique half-graben inversion of the Mesozoic Neuquén Rift in the Malargüe Fold and Thrust Belt, Mendoza, Argentina: New insights from analogue models

The Malargüe fold and thrust belt, located in the Andean mountains between 34°S and 36°30′S, formed in response to contraction during Cenozoic times. Its structural style and geometry was controlled by the Mesozoic rift system that formed the Neuquén basin in west-central Argentina. The rift archite...

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Detalles Bibliográficos
Publicado:	2008
Materias:	Analogue modeling Malargüe fold Oblique inversion Thrust belt (1 1 1) orientation Argentina Cenozoic cross sectioning Early Jurassic Fold-and-thrust belts Half-graben normal faults Rift systems Structural styles Structural trends Subsurface data Triassic Computer networks Mathematical models Neon Tectonics analog model fold and thrust belt graben inversion tectonics lineament Mesozoic normal fault oblique fault rift zone rifting Malargue Mendoza Neuquen South America Capsicum pubescens
Acceso en línea:	https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_01918141_v30_n7_p839_Yagupsky http://hdl.handle.net/20.500.12110/paper_01918141_v30_n7_p839_Yagupsky
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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