DEPOCENTROS CENOZOICOS DE LA CUENCA AUSTRAL EN EL CONTEXTO DE LA APERTURA DEL PASAJE DE DRAKE (Record no. 196195)
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| 000 -LEADER | |
|---|---|
| fixed length control field | 02963nmc a2200229 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 | Simposio sobre la Exploración Offshore en el Sector Sur del Margen Atántico Sudamericano |
| 245 00 - TITULO | |
| Título | DEPOCENTROS CENOZOICOS DE LA CUENCA AUSTRAL EN EL CONTEXTO DE LA APERTURA DEL PASAJE DE DRAKE |
| 270 ## - FECHA DE CARGA | |
| Fecha de carga | 10/11/2023 ; 10/11/2023 |
| 300 ## - DESCRIPCION FISICA | |
| Otra extensión | 10 p. ; 121-130 |
| 520 ## - RESUMEN, ETC | |
| Resumen | Cretaceous-Cenozoic interaction between the South America and Antarctica plates has been a major driver of kinematics in the Southernmost Andes, imprinting extensional and strikeslip deformation within the foreland in Tierra del Fuego. Late Cretaceous basin inversion and transpression along the Beagle channel was due to their left-lateral relative displacement. Orogen building continued during the Paleogene, together with progression of sedimentation in the associated Austral-Malvinas marine foreland basin system and depocenters migrations. The Eocene early opening of the Drake passage due to Antarctica separation, involved the combination of strike-slip and extensional tectonics, superposed to the previously consolidated orogen. A series of latest Paleocene–early Eocene fault-related extensional depocenters can be recognized in the Austral and Malvinas basins, which represent a direct indication of continental lithospheric stretching preceding the opening of embryonic basins in the West Scotia Sea. A middle-late Eocene compressional stage followed, characterized by rapid migration of the orogenic front and establishment of a widespread wedge-top depocenter. Since the Oligocene inception of oceanic spreading in the West Scotia Sea, strike-slip deformation has dominated, concentrated along the North Scotia ridge-Magallanes-Fagnano fault zone. As a result, late Cenozoic continental pull-apart basins are registered in a hinterland position. Coeval retroarc Miocene sedimentation includes an important continental volcaniclastic component and distributary system funneling sediments to deep marine basins. In this context, tectonic loading, dynamic subsidence, and transtension/pullapart extension seems to be superposed; alternatively, they may be partitioned processes and geographically distributed. We present a synthesis of this history of changing tectonic regimes and depocenters migration in the southernmost Andes and the Austral basin from and discuss the implication of new detrital zircons provenance data. |
| 773 ## - CORRECCIÓN | |
| Partes relacionadas | |
| 942 ## - DESC. DE MATERIAL | |
| Tipo de item KOHA | Congresos (trabajos presentados) |
| 100 1# - RESPONSABLE PERSONAL | |
| Apellido, Nombre | Ghiglione, Matías C. |
| 9 (RLIN) | 58726 |
| 100 1# - RESPONSABLE PERSONAL | |
| Apellido, Nombre | Gallardo-Jara, Rocío |
| 9 (RLIN) | 61497 |
| 100 1# - RESPONSABLE PERSONAL | |
| Apellido, Nombre | Calderón, Mauricio |
| 9 (RLIN) | 61498 |
| 111 2# - AUTORIDAD DE CONGRESO | |
| Nombre de congreso | Congreso de Exploración y Desarrollo de Hidrocarburos (11er : 2022 nov. 8 - 11 : Mendoza) |
| 9 (RLIN) | 61064 |
| 856 ## - LINK | |
| Link | <a href="https://biblioteca.iapg.org.ar/ArchivosAdjuntos/Conexplor2022/Simp.Explor.Offshore/offshore07.pdf">https://biblioteca.iapg.org.ar/ArchivosAdjuntos/Conexplor2022/Simp.Explor.Offshore/offshore07.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 virtual | Biblioteca virtual | 068.82 553.28 C62 15730 | 06/03/2026 | 200068613 | 068.82 553.28 C62 15730 | 200068613 | 06/03/2026 | Archivo electrónico |
