Atributos de la diferencia de angle stacks como indicadores de gas (Record no. 128404)

MARC details
000 -LEADER
fixed length control field 02680nmc a2200241 4500
008 - CÓDIGOS DE INFORMACIÓN DE LONGITUD FIJA - INFORMACIÓN GENERAL
Campo de control de longitud fija 260224s xxu esp
041 ## - IDIOMA
Idioma Español
082 ## - CLASIFICACIÓN DEWEY
Número de clasificación 068.82 553.28 C62 2018 0015644
245 00 - TITULO
Título Atributos de la diferencia de angle stacks como indicadores de gas
270 ## - FECHA DE CARGA
Fecha de carga 30/06/2022 ; 21/02/2019
300 ## - DESCRIPCION FISICA
Otra extensión 13 p. ; 435-448
520 ## - RESUMEN, ETC
Resumen It’s well known that when a seismic wave propagates through Earth’s interior, its energy diminishes due to spherical divergence, scattering, intrinsic absorption and reflection at interfaces where there are changes in the rock properties. There are a variety of factors such as geological structure, layer thickness, lithology, and pore fluid properties that affect the amplitude and frequency of the reflected seismic wave. Once the wave field returns to the surface, it also brings back the information related to stratigraphic features, rock property changes and hydrocarbon accumulations.The Amplitude Variation with Offset (AVO) has been widely used in the oil industry as a tool to predict gas presence. Because of that it is common nowadays to have a set of 3D data processed as Near-Middle-Far Angle/Offset Stack that allow a better picture of the AVO information in the seismic data.The present work shows an effective predictive tool that uses the amplitude and frequency content of the partial angle stack difference to detect gas accumulations zones.We are going to show the evolution of a simple workflow with which, once verified the feasibility of the use of the partial angle stack datasets we’ll be able to generate two seismic cubes, the Root Mean Square (RMS) Amplitude and the Instantaneous Frequency of the Far Angle and Near Angle Stack difference. After that we use cross plot that let us correlate ranges of RMS Amplitude and Instantaneous Frequency with the wells’s petrophysics and obtain geobodies containing the same reservoir characteristics than the wells used as input to the model.Finally we are going to show the results of three wells drilled in the North Flank of Cuenca del Golfo San Jorge whose proposals where based in this methodology as a predictive tool to find reservoirs with commercial quantities of gas.
773 ## - CORRECCIÓN
Partes relacionadas
942 ## - DESC. DE MATERIAL
Tipo de item KOHA Congresos (trabajos presentados)
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Van Haaster, Christian J.J.
9 (RLIN) 653
111 2# - AUTORIDAD DE CONGRESO
Nombre de congreso Simposio de Geofísica (2018 nov. 5 - 9 : Mendoza)
9 (RLIN) 561
650 #0 - MATERIA
Término tópico Gas
9 (RLIN) 654
650 #0 - MATERIA
Término tópico Cuenca del Golfo San Jorge
9 (RLIN) 655
650 #0 - MATERIA
Término tópico Formación D129
9 (RLIN) 656
856 ## - LINK
Link <a href="https://biblioteca.iapg.org.ar/ArchivosAdjuntos/Conexplor2018/SGeof/1684.pdf">https://biblioteca.iapg.org.ar/ArchivosAdjuntos/Conexplor2018/SGeof/1684.pdf</a>
Holdings
Biblioteca propietaria Biblioteca actual Ubicación Fecha de adquisición Inventario Total de préstamos Signatura topográfica Inventario Fecha de carga Tipo de item KOHA
Biblioteca virtual Biblioteca virtual 068.82 553.28 C62 2018 0015644 02/03/2026 200064901   068.82 553.28 C62 2018 0015644 200064901 02/03/2026 Archivo electrónico


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