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082 _a068.82 553.28 C62 2014 0015581
245 0 0 _aCaracterización de discontinuidades sísmicas: cálculo y procesos de atributos sobre amplitud
270 _a15/05/2020 ; 23/03/2017
300 _a17 p.
520 _aSeismic characterization of breaks: Calculation and process attributes on amplitude The study of conventional reservoirs, as the new unconventional ones, emphasizes analysis on several approaches. Those include the research of the depositional environment and geological properties, and the analysis of concepts such as organic matter content, reservoir pore pressure, rock brittleness, etc. In both cases, fault and fracture interpretation and characterization have an important role depending on the purpose and kind of the investigated reservoir. For Conventional cases, their identification is useful for delineating areas of interest. On the other hand, for Unconventional ones these processes optimize the well location and completion. Seismic discontinuities, represented as vertical and horizontal displacements, flexure deformations and/or seismic reflector variations, are closely related to geological faults, fractures, or stratigraphic features of a given geologic environment. The present paper focuses on the estimation of 3D geometric attributes for characterizing discontinuities of seismic and subseismic scale fractures associated to geological fractures and faults. Calculated attributes were: curvature, coherency, Volume Amplitude Technique (TecVA) and TecVA variations. An analysis of its effects and contributions to the seismic interpretation is presentedt.
773 _g
942 _cCONGTP
100 1 _aAtencio, Mario R.
_9616
100 1 _aSpäth, Federico G. E.
_9617
100 1 _aRendon, Daniel
_956302
111 2 _aCongreso de Exploración y Desarrollo de Hidrocarburos (9no. : 2014 nov. 3-7 : Mendoza)
_954287
111 2 _aSimposio de Geofísica "La geofísica : puentes de integración" (2014 nov. 3-7 : Mendoza)
_956096
999 _c190158
_d190158
856 _uhttps://biblioteca.iapg.org.ar/ArchivosAdjuntos/CONEXPLOR2014/Simposiodegeofisica/123-Caracterizacion-de-discontinuidades.pdf