Análisis diagnético y estructural en la formación Tunas Pozo Pang001. Pérmico de la Cuenca de Claromecó. Sierras Australes de la Provincia de Buenos Aires, Argentina (Record no. 189827)
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| 000 -LEADER | |
|---|---|
| fixed length control field | 02715nmc a2200241 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 | Análisis diagnético y estructural en la formación Tunas Pozo Pang001. Pérmico de la Cuenca de Claromecó. Sierras Australes de la Provincia de Buenos Aires, Argentina |
| 270 ## - FECHA DE CARGA | |
| Fecha de carga | 10/11/2016 ; 10/11/2016 |
| 300 ## - DESCRIPCION FISICA | |
| Otra extensión | 17 p. |
| 520 ## - RESUMEN, ETC | |
| Resumen | Structural and Diagenetic analysis of Tunas Formation, PANG0001 well. Permian of Claromecó Basin, Sierras Australes fold and thrust belt, Buenos Aires province, Argentina The Tunas Formation (Permian, Harrington 1947) outcrops in Sierras Australes of Buenos Aires Province and continues to the east in Claromecó Basin as subsurface record. In order to know about diagenesis level, structural evolution and tectonic context, petrographic analysis on well PANG0001 coal samples and magnetic suceptibility anisotropy (MSA) studies of outcropping samples were made. Coals are formed by collovitrinite and gelovitrinite (Vitrinite Group) belts, alternate with fusinite (Inertinite Group) belts. The values of vitrinite reflectance are between 1,3 and 2,38% R0, wich allow us to classify the coals as semianthracitic to low volatile bituminous. According to this, the Tunas Formation reaches the methane gas to wet to condensate gases window generation. The Kmax axes of AMS ellipsoids show a NW-SE direction showing a maximum stress direction from SW-NE. The Kmin axes, with a SW-NE strike, are in horizontal positions at west progressively changing to vertical positions at east, while the anisotropy magnitude decreases toward the East. All these aspects indicate a progression of the magnetic fabric, from a tectonic imprint to a sedimentary fabric, evidencing a decreasing of the deformation to the East while principal compressive stress comes from SW. This research takes into account different methods and allows a good knowledge about diagenesis degree and deformation features recording. Results inform that the Tunas Formation have reached the catagenesis-metagenesis zone and that can be characterized as a potential component of an oil/gas/coal system. |
| 773 ## - CORRECCIÓN | |
| Partes relacionadas | |
| 942 ## - DESC. DE MATERIAL | |
| Tipo de item KOHA | Congresos (trabajos presentados) |
| 100 1# - RESPONSABLE PERSONAL | |
| Apellido, Nombre | Arzadún, Guadalupe |
| 9 (RLIN) | 982 |
| 100 1# - RESPONSABLE PERSONAL | |
| Apellido, Nombre | Nela Tomezzoli, Renata |
| 9 (RLIN) | 55755 |
| 100 1# - RESPONSABLE PERSONAL | |
| Apellido, Nombre | Cisternas, María Eugenia |
| 9 (RLIN) | 55756 |
| 100 1# - RESPONSABLE PERSONAL | |
| Apellido, Nombre | Cesaretti, Nora Noemí |
| 9 (RLIN) | 981 |
| 100 1# - RESPONSABLE PERSONAL | |
| Apellido, Nombre | Fortunatti, Natalia |
| 9 (RLIN) | 55757 |
| 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/CONEXPLOR2014/481-Analisisdiagenetico.pdf">https://biblioteca.iapg.org.ar/ArchivosAdjuntos/CONEXPLOR2014/481-Analisisdiagenetico.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 | 200062073 | CD I116 64 0015469 | 200062073 | 06/03/2026 | Archivo electrónico |
