A GEOCHEMICAL POTENTIAL REVIEW OF THE TINDOUF BASIN , ALGERIAN SAHARA (Record no. 133510)

MARC details
000 -LEADER
fixed length control field 02432nmc 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 CD W938 1 0013960
210 ## - TITULO ABREVIADO
Título abreviado WPC (16th.)
245 00 - TITULO
Título A GEOCHEMICAL POTENTIAL REVIEW OF THE TINDOUF BASIN , ALGERIAN SAHARA
270 ## - FECHA DE CARGA
Fecha de carga 12/09/06 ; 26/08/2003
300 ## - DESCRIPCION FISICA
Otra extensión 11 p.
520 ## - RESUMEN, ETC
Resumen Resumen del autor, extraído del trabajo. The Tindouf basin which is forming at the present time a vast E-W striking depression is bound in the north by the Anti-Atlas belt, in the south by the Eglab shield, in the East by the Boubernous arch with an extension to the West, beyond the Algerian border. The Tindouf basin, spreading over some 100.000 sq km , is quite underexplored, since only 11 wells were drilled there. Some gas shows were encountered in the sandstones of EAN-1 (Ordovician), Htn-1 (lower Devonian) and NG-1 (Tournaisian - Strunian). The main reservoir horizons are: the sandstones and quartzites of Cambrian and Ordovician, the sandstones of lower Devonian (Emsian) and of Tournaisian- Strunian. All the horizons likely to form source-rocks were sampled and analysed. The northern flank of the basin shows a higher organic matter ratio with the following values: - The Ordovician, of about 2000 m thick, holds clay horizons (clays of Feijas and Ktaoua, 670m and 300m thick, respectively) are organic-matter rich with a T.O.C of 2% in HMA-1. - The Upper Silurian, generally represented by the Famennian and Strunian clays, is 1600m thick with T.O.C of up 2.32% in HMA-1. As to the south flank, the source-rocks become more detritic and poorer in organic matter. - The present geothermal gradient ranges from 35.7°C/km in the north (IGA-1) to 26.3°C/Km in the south. - All the horizons are overmature (dry gas and more) in the north flank However, the maturity is decreasing progressively towards the southern flank, since it is still in the oil-phase. The southern flank of the basin is a hydrocarbon prospective area where exploration activity will certainly lead to new traps highlight, related to structures and noses.
773 ## - CORRECCIÓN
Partes relacionadas v. 2, p. 76-86
942 ## - DESC. DE MATERIAL
Tipo de item KOHA Congresos (trabajos presentados)
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Malla, M.S.
9 (RLIN) 9733
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Takherist, D.
9 (RLIN) 9734
111 2# - AUTORIDAD DE CONGRESO
Nombre de congreso World Petroleum Congress (16th. : 2000 jun. 11-15 : Calgary, Alberta, Canada)
9 (RLIN) 34
700 1# - OTRA AUTORIDAD PERSONAL
Nombre Takherist, D.
9 (RLIN) 9734
800 1# - RESPONSABLE EDICION
Nombre Malla, M.S.
9 (RLIN) 9733
Holdings
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 W938 1 0013960 04/03/2026 200005999   CD W938 1 0013960 200005999 04/03/2026 Archivo electrónico


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