Remanentes depositacionales del Grupo Neuquén (Cretácico Superior) en Cuenca Neuquina, Argentina: su importancia en la caracterización del reservorio (Record no. 189779)
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| 000 -LEADER | |
|---|---|
| fixed length control field | 02411nmc a2200205 4500 |
| 008 - CÓDIGOS DE INFORMACIÓN DE LONGITUD FIJA - INFORMACIÓN GENERAL | |
| Campo de control de longitud fija | 260224s xxu |
| 082 ## - CLASIFICACIÓN DEWEY | |
| Número de clasificación | CD I116 64 0015469 |
| 245 00 - TITULO | |
| Título | Remanentes depositacionales del Grupo Neuquén (Cretácico Superior) en Cuenca Neuquina, Argentina: su importancia en la caracterización del reservorio |
| 270 ## - FECHA DE CARGA | |
| Fecha de carga | 21/10/2016 ; 21/10/2016 |
| 300 ## - DESCRIPCION FISICA | |
| Otra extensión | 25 p. |
| 520 ## - RESUMEN, ETC | |
| Resumen | Neuquén Group (Upper Cretaceous) residual deposits in Neuquén Basin, Argentina: importance in reservoir characterization In this paper features of small and medium scale contributing to the identification of geometries and relations in subsurface reservoirs are illustrated considering the relevance in the exploration and production of hydrocarbons. This type of depositional remnants of lithostratigraphic units of the Neuquén Group containing strata exhumed reservoirs or migration (carrier beds) are characterized. During the late stages of underfilled basin, low accommodation and under high pulsed supply, there is a tendency to the preservation of the depositional geometry. This is common in Candeleros and Huincul Formations (Río Limay Subgroup) and Bajo de la Carpa Formation (Río Colorado Subgroup). During the early stages of underfilled basin in Cerro Lisandro Formation (Río Limay Subgroup), of deltaic medium-scale accommodation remnants, lacustrine deposits isolated on acting as seals in the deep basin (foredeep) were generated. While in the area of peripheral basin, under high accommodation space favored the preservation of aeolian dunes and generation erosional valleys that affect the overlain Huincul Formation erosional remnants forming. The erosional remnants are common as medium-scale remnants in Portezuelo Formation as a result of deposition under low accommodation, during the period of underfilled basin. Under similar conditions the Bajo de la Carpa Formation generates erosional aeolian remnants and excavation of small-scale fluvial valleys in Plottier Formation. |
| 773 ## - CORRECCIÓN | |
| Partes relacionadas | |
| 942 ## - DESC. DE MATERIAL | |
| Tipo de item KOHA | Congresos (trabajos presentados) |
| 100 1# - RESPONSABLE PERSONAL | |
| Apellido, Nombre | Asurmendi, Estefanía |
| 9 (RLIN) | 935 |
| 100 1# - RESPONSABLE PERSONAL | |
| Apellido, Nombre | Sánchez, María Lidia |
| 9 (RLIN) | 917 |
| 111 2# - AUTORIDAD DE CONGRESO | |
| Nombre de congreso | Congreso de Exploración y Desarrollo de Hidrocarburos (9no. : 2014 nov. 3-7 : Mendoza) |
| 9 (RLIN) | 54287 |
| 856 ## - LINK | |
| Link | <a href="https://biblioteca.iapg.org.ar/ArchivosAdjuntos/CONEXPLOR2014/337-Remanentesdepositacionales.pdf">https://biblioteca.iapg.org.ar/ArchivosAdjuntos/CONEXPLOR2014/337-Remanentesdepositacionales.pdf</a> |
| Biblioteca propietaria | Biblioteca actual | Ubicación | Fecha de adquisición | Inventario | Total de préstamos | Signatura topográfica | Inventario | Fecha de carga | Tipo de item KOHA |
|---|---|---|---|---|---|---|---|---|---|
| Biblioteca Alejandro Angel Bulgheroni | Biblioteca Alejandro Angel Bulgheroni | CD I116 64 0015469 | 06/03/2026 | 200062025 | CD I116 64 0015469 | 200062025 | 06/03/2026 | Archivo electrónico |
