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ANÁLISIS DE LA EVOLUCIÓN DEL LINEAMIENTO ESTRUCTURAL DE LOMA LA LATA OESTE - EL CORDÓN - LINDERO ATRAVESADO A PARTIR DE NUEVOS DATOS SÍSMICOS PARA LA FORMACIÓN VACA MUERTA

By: Description: 20 p. ; 179-198DDC classification:
  • 068.82 553.28 C62 15730
Online resources: Summary: This paper presents a new interpretation of the deformation events linked to the structural evolution of the Lindero Atravesado – El Cordón – Loma La Lata Oeste transcurrent fault system. It’s a WNW-ESE trending narrow zone that extends about 100 km along the southern border of the Neuquén Basin. High quality 3D seismic data allowed the definition of a detailed fault pattern and a 2D geomechanical restoration was used to simulate failures and deformation patterns in different time intervals allowing the determination of active and non-active faults as well as folds appearance and evolution. For the determination of stress orientation and the stress field, GPlates software was used. The obtained results indicate a complex displacement field and stress rotation, from deeper levels to Vaca Muerta Formation terms.
Item type: Congresos (trabajos presentados) List(s) this item appears in: Conexplo 2022
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This paper presents a new interpretation of the deformation events linked to the structural evolution of the Lindero Atravesado – El Cordón – Loma La Lata Oeste transcurrent fault system. It’s a WNW-ESE trending narrow zone that extends about 100 km along the southern border of the Neuquén Basin. High quality 3D seismic data allowed the definition of a detailed fault pattern and a 2D geomechanical restoration was used to simulate failures and deformation patterns in different time intervals allowing the determination of active and non-active faults as well as folds appearance and evolution. For the determination of stress orientation and the stress field, GPlates software was used. The obtained results indicate a complex displacement field and stress rotation, from deeper levels to Vaca Muerta Formation terms.



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