| 000 | 01752nmc a2200229 4500 | ||
|---|---|---|---|
| 005 | 20260520010443.0 | ||
| 008 | 260224s xxu | ||
| 040 | _aBAAB | ||
| 082 | _a068.82 553.28 C62 15730 | ||
| 100 | 1 | _aRoth, Rocío | |
| 100 | 1 | _aManceda, René | |
| 100 | 1 | _aMerchán Jaimes, Vladimir | |
| 100 | 1 | _aRossi, Juan | |
| 111 | 2 | _aCongreso de Exploración y Desarrollo de Hidrocarburos (11er : 2022 nov. 8 - 11 : Mendoza) | |
| 245 | 0 | 0 | _aANÁLISIS 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 |
| 270 | _a11/08/2023 ; 11/08/2023 | ||
| 300 | _a20 p. ; 179-198 | ||
| 520 | _aThis 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. | ||
| 856 | _uhttps://biblioteca.iapg.org.ar/ArchivosAdjuntos/Conexplor2022/GeologíaEstructural/geologia-estructural-y-tectonica09.PDF | ||
| 942 | _cCONGTP | ||
| 945 | _aDominguez, Silvia | ||
| 999 |
_c195910 _d195910 |
||