Basin dynamics and petroleum potential of the Eocene series in the gulf of Gabes, Tunisia (Record no. 182168)
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| 000 -LEADER | |
|---|---|
| fixed length control field | 02451nab a2200205 4500 |
| 008 - CÓDIGOS DE INFORMACIÓN DE LONGITUD FIJA - INFORMACIÓN GENERAL | |
| Campo de control de longitud fija | 260224s2010 xxu |
| 245 00 - TITULO | |
| Título | Basin dynamics and petroleum potential of the Eocene series in the gulf of Gabes, Tunisia |
| 260 ## - PUBLICACION, DISTRIBUCION, ETC | |
| Lugar de publicación, distribución, etc. | |
| Nombre de publicador, distribuidor, etc. | |
| Fecha de publicación, distribución, etc. | dic. 2010 |
| 270 ## - FECHA DE CARGA | |
| Fecha de carga | 30/05/2011 ; 30/05/2011 |
| 300 ## - DESCRIPCION FISICA | |
| Otra extensión | 14 p. ; 114-128 |
| 520 ## - RESUMEN, ETC | |
| Resumen | Transcripción del resumen del autor: The sedimentary series in the study area includes marls with limestone interbeds of the Upper Maastrichtian–Paleocene, Ypresian Nummulitid-rich limestones which grew laterally into limestones and black shales, and overlying Upper Eocene marl and fossiliferous limestones. Well correlations and outcrop data point to sedimentary sequences vary considerably in lithofacies and thicknesses, with significant gaps. Seismic stratigraphical modeling basing on petrologic evidence from cores and well-cuttings, as well as wireline log details (sonic and gamma ray) helps recognize three main supersequences SS1 to SS3. The supersequence SS1 (Upper Maastrichtian–Paleocene) has rather oblique seismic configurations testifying to prograding entities during periods of sea-level rise. The supersequence SS2 (Ypresian) is comprised of platform to basin carbonates with transparent seismic facies, local high amplitudes and onlapping configurations relevant to drawdown and aggrading sequences. The third supersequence SS3 (Upper Eocene) shows transparent seismic facies, and also continuous reflections with high amplitudes, which tend to indicate strata deposited under influential subsidence. The geometry of sequences, seismic facies and reactivating faults in the mid-gulf, lend support to a depositional model evolving from tectonically induced slope with bathymetry increasing northeastwards. The Eocene petroleum system associates black shales with high TOC contents (0.15–4%) and elevated HI values (up to 16 kg/t HC), and a porous Nummulite-bearing limestone reservoirs; these were early sealed by broadly spread Upper Eocene clays, whereas, source-rock maturation and hydrocarbon migration might have occurred during the Tortonian–Pliocene Atlassic compression. |
| 581 ## - ESTADO DE COLECCIÓN | |
| Estado de colección | 1-2 |
| 773 0# - CORRECCIÓN | |
| Título | Journal of Petroleum Science & Engineering |
| Partes relacionadas | 75 |
| 942 ## - DESC. DE MATERIAL | |
| Tipo de item KOHA | Artículo de Revista |
| 100 1# - RESPONSABLE PERSONAL | |
| Apellido, Nombre | Taktak, Fatma |
| 9 (RLIN) | 50063 |
| 100 1# - RESPONSABLE PERSONAL | |
| Apellido, Nombre | Kharbachi, Samir |
| 9 (RLIN) | 50064 |
| 100 1# - RESPONSABLE PERSONAL | |
| Apellido, Nombre | Bouaziz, Samir |
| 9 (RLIN) | 50065 |
| 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 | 200054208 | 200054208 | 05/03/2026 | Artículo de Revista |
