Kinematic analysis of a transtensional fault system: The Atuel depocenter of the Neuquén basin, southern Central Andes, Argentina

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The Atuel depocenter of the Neuquén basin originated as an Upper Triassic to Lower Jurassic rift system, later inverted during the Andean contractional deformation. In order to study the extensional architecture and the kinematic evolution of this depocenter, we collected a large amount of field and...

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Detalles Bibliográficos
Autores principales: Bechis, F., Giambiagi, L., García, V., Lanés, S., Cristallini, E., Tunik, M.
Formato: JOUR
Materias:
Central Andes
Kinematic analysis
Neuquén basin
Oblique rift
Transtension
Argentina
Bimodal distribution
Facies distribution
Fault system
Fourth order
General trends
Jurassic
Kinematic evolution
Kinematic indicators
Lithospheric
Normal faults
Paleozoic
Rift systems
Second orders
Shear zone
Structural data
Sub-surfaces
Subbasins
Syn-rift
Upper Triassic
Angular distribution
Geochronology
Kinematics
depocenter
extensional tectonics
kinematics
oblique fault
rift zone
tectonic evolution
transtension
Andes
Neuquen Basin
Acceso en línea:http://hdl.handle.net/20.500.12110/paper_01918141_v32_n7_p886_Bechis
Aporte de:
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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