Facies piroclásticas y diagénesis de la formación Río Blanco en el depocentro Tupungato, Cuenca Cuyana (Record no. 189820)
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| 000 -LEADER | |
|---|---|
| fixed length control field | 02198nmc 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 | Facies piroclásticas y diagénesis de la formación Río Blanco en el depocentro Tupungato, Cuenca Cuyana |
| 270 ## - FECHA DE CARGA | |
| Fecha de carga | 10/11/2016 ; 10/11/2016 |
| 300 ## - DESCRIPCION FISICA | |
| Otra extensión | 21 p. |
| 520 ## - RESUMEN, ETC | |
| Resumen | Pyroclastic facies and diagenesis of Río Blanco formation, Tupungato depocenter, Cuyana Basin Related to important petroleum accumulations, a well-known record of Triassic has been preserved in Cuyana Basin. Main rifting faults trend and delineate the Tupungato depocenter, located on the Southwest flank of Cacheuta sub-basin. The most remarkable feature in this sector is the uncoupling effect recognized in 3D subsurface data between the faulted Triassic strata and the folded Meso- Cenozoic deposits. In this area of study the most important reservoirs are allocated on Río Blanco formation (Late Triassic). Integrated subsurface information is herein presented in order to discuss the importance of pyroclastic products in the constraint of the sedimentary infilling of this depocenter, during the deposition of Río Blanco formation. Based on an unconformity, two different sedimentary units are proposed: Lower Rio Blanco (RBI) and Upper Rio Blanco (RBS) sequences. We suggest that RBS sequence is the result of a proximal volcanic system interacting with a lacustrine system. It is also considered analcime as the most important diagenetic product that determines reservoir quality. We suggest that the current location of Chañares Herrados oil field, Anchayuyo-Chañares Sur transfer zone and Puesto Pozo Cercado-Cruz Negra complex were part a an important Triassic volcanic system reactivated during Jurassic and Cretaceous times. |
| 773 ## - CORRECCIÓN | |
| Partes relacionadas | |
| 942 ## - DESC. DE MATERIAL | |
| Tipo de item KOHA | Congresos (trabajos presentados) |
| 100 1# - RESPONSABLE PERSONAL | |
| Apellido, Nombre | Gómez, Gustavo A. |
| 9 (RLIN) | 55739 |
| 100 1# - RESPONSABLE PERSONAL | |
| Apellido, Nombre | Stahlschmidt, Erico H. |
| 9 (RLIN) | 19311 |
| 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/CONEXPLOR2014/409-Faciespiroclasticas.pdf">https://biblioteca.iapg.org.ar/ArchivosAdjuntos/CONEXPLOR2014/409-Faciespiroclasticas.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 | 200062066 | CD I116 64 0015469 | 200062066 | 06/03/2026 | Archivo electrónico |
