ANÁLISIS DE FRACTURAS NATURALES Y BANDAS DE DEFORMACIÓN EN CORONAS E IMÁGENES DE POZO, Y SU RELACIÓN CON LA ESTIMULACIÓN Y PRODUCTIVIDAD DE POZOS. GRUPO CUYO, YACIMIENTO RÍO NEUQUÉN. ARGENTINA (Record no. 195638)

MARC details
000 -LEADER
fixed length control field 03487nmc a2200253 4500
008 - CÓDIGOS DE INFORMACIÓN DE LONGITUD FIJA - INFORMACIÓN GENERAL
Campo de control de longitud fija 260224s xxu
082 ## - CLASIFICACIÓN DEWEY
Número de clasificación 068.82 553.28 C62 15730
210 ## - TITULO ABREVIADO
Título abreviado Desarrollo y Sustentabilidad
245 00 - TITULO
Título ANÁLISIS DE FRACTURAS NATURALES Y BANDAS DE DEFORMACIÓN EN CORONAS E IMÁGENES DE POZO, Y SU RELACIÓN CON LA ESTIMULACIÓN Y PRODUCTIVIDAD DE POZOS. GRUPO CUYO, YACIMIENTO RÍO NEUQUÉN. ARGENTINA
270 ## - FECHA DE CARGA
Fecha de carga 21/04/2023 ; 21/04/2023
300 ## - DESCRIPCION FISICA
Otra extensión 24 p. ; 1-24
520 ## - RESUMEN, ETC
Resumen Since the beginning of tight-gas sandstone development in the Río Neuquén field, natural fractures have been suspected to influence production and hydraulic fracture stimulation. In this paper, we analyze available information regarding natural fractures using core, image logs, and outcrop analogs of the Punta Rosada and Lajas Formations to evaluate these possible effects. The Rio Neuquén field is located in the Neuquén basin gulf and at the time of submission of this study, contained 50 wells (16 with image logs and 6 with core) targeting these two tight-gas sandstone reservoirs. The reservoirs consist mostly of low-porosity and permeability, overpressured, feldespathic litharenites and lesser conglomerates overlaying source rocks of Los Molles Fm. The reservoirs are ~3000 ft thick forming an anticline with closure in three directions that terminates against a fault to the NNE. Natural fractures usually show slickensides indicating shear and occur mostly in pelitic intervals, whereas sandstone and conglomeratic intervals are dominated by deformation bands. Deformation bands in core and outcrop analogs are mostly cataclastic, with abundant clay mineral and/or oxide cement, angular clasts, and important grain-size reduction resulting in barriers to fluid flow. Most deformation bands are subvertical, but in some cores several hundred, bed-parallel deformation bands have been observed arranged in meter-sized clusters that correspond with sand-dominated lithofacies. In some wells, the azimuth of natural fractures and deformation bands can be correlated with nearby faults, suggesting a genetic relationship. Because of their potential impact on reservoir permeability, being able to identify natural fractures and, specially, deformation bands in image logs is of utter importance. Although both types of structural discontinuities have been inferred in image logs, detecting and distinguishing between the two is challenging. Deformation bands typically show as conductive planes due to the presence of clay, oxides, pyrite and/or bitumen along them. Moreover, the differential presence of hydrocarbons on both sides of the bands can facilitate their detection. From a productivity standpoint, we conclude that natural fractures in pelites reactivate and cause fluid loss along hydraulic fractures during stimulation, whereas deformation bands are most likely responsible for the reduced fluid flow observed in some wells.
773 ## - CORRECCIÓN
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856 ## - LINK
Link <a href="https://biblioteca.iapg.org.ar/ArchivosAdjuntos/Conexplor2022/Desarr-y-Sustent/desarrollo-y-sustentabilidad01.PDF">https://biblioteca.iapg.org.ar/ArchivosAdjuntos/Conexplor2022/Desarr-y-Sustent/desarrollo-y-sustentabilidad01.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 15730 06/03/2026 200068052   068.82 553.28 C62 15730 200068052 06/03/2026 Archivo electrónico


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