Basin evolution of the Lurestan region inthe Zagros fold-and-thrust belt, Iran (Record no. 168977)
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| 000 -LEADER | |
|---|---|
| fixed length control field | 02112nab a2200193 4500 |
| 008 - CÓDIGOS DE INFORMACIÓN DE LONGITUD FIJA - INFORMACIÓN GENERAL | |
| Campo de control de longitud fija | 260224s2009 xxu |
| 100 1# - RESPONSABLE PERSONAL | |
| Apellido, Nombre | Farzipour-Saein, A. |
| 9 (RLIN) | 40270 |
| 245 00 - TITULO | |
| Título | Basin evolution of the Lurestan region inthe Zagros fold-and-thrust belt, Iran |
| 260 ## - PUBLICACION, DISTRIBUCION, ETC | |
| Fecha de publicación, distribución, etc. | Ene. 2009 |
| 270 ## - FECHA DE CARGA | |
| Fecha de carga | 2009-02-04 ; 2009-02-04 |
| 300 ## - DESCRIPCION FISICA | |
| Otra extensión | 15 p. ; 5-20 |
| 520 ## - RESUMEN, ETC | |
| Resumen | Transcripción del resumen publicado por el autor: The evolution of the central part of the Lurestan region in the Zagros fold-and-thrust belt has been studied using newly generated isopach maps for different time intervals between the Late Cretaceous and the Miocene. The study was based on existing geological maps, gravity data, measured stratigraphic surface sections, original field work and well data. Understanding the processes which have influenced facies and thickness variations in the study area will have a significant impact on future hydrocarbon exploration. Cenomanian carbonates assigned to the Sarvak Formation, the main reservoir unit in the study area, are composed of both pelagic and neritic facies. These facies occur along the roughly north-south trending "Anaran lineament" interpreted to represent a palaeohigh, which influenced patterns of sedimentation in the Cretaceous-Tertiary. The palaeohigh formed as a result of the reactivation of a basement lineament in the Late Cretaceous. The continuing influence of this lineament on patterns of sedimentation during Oligocene ' early Miocene time is indicated by a range of evidence including the presence of clinoform geometries. Analysis of sedimentary thicknesses in the Zagros foreland basin between the Late Cretaceous and the early Miocene indicates progressive SWward migration of the depocentre. Late Cretaceous ophiolite obduction and plate margin convergence exerted a major influence on stratigraphic architecture, and controlled depocentre migration and foreland basin evolution |
| 581 ## - ESTADO DE COLECCIÓN | |
| Estado de colección | 1 |
| 650 #0 - MATERIA | |
| Término tópico | Irán |
| 9 (RLIN) | 5182 |
| 773 0# - CORRECCIÓN | |
| Título | Journal of Petroleum Geology |
| Partes relacionadas | 32 |
| 942 ## - DESC. DE MATERIAL | |
| Tipo de item KOHA | Artículo de Revista |
| Fuente de clasificación | Dewey Decimal Classification |
| Biblioteca propietaria | Biblioteca actual | Fecha de adquisición | Inventario | Total de préstamos | Inventario | Fecha de carga | Tipo de item KOHA |
|---|---|---|---|---|---|---|---|
| Biblioteca Alejandro Angel Bulgheroni | Biblioteca Alejandro Angel Bulgheroni | 05/03/2026 | 200043766 | 200043766 | 05/03/2026 | Artículo de Revista |
