Kibuku area is located within Semlik sub basin, the southern part of the Albertine Graben in the western branch of the East Africa rift system. The rift flanks are underlined by basement rocks such as gneisses, quartzite, amphibolite, schist, and granitic-gneisses. Kibuku area is further divided into six formations namely Kisegi, Kasande, Kakara, Oluka, Nyaburogo and Katorogo, from oldest to youngest respectively. To delineate deposition environment and hydrocarbon potential; geologic mapping, grain size analysis, palaeocurrent analysis and sedimentologic logging.The main Syn rift Lithology encountered include clays, sands, silts, iron bands, pebbles, and conglomerates while Pre-rift Lithology includes schist, granitic-gneisses, mafic intrusions, amphibolite, gneisses and quartz veins. The structures included joints, faults, foliation (mainly in metamorphic rocks) and laminations, mega-ripple marks, tabular beds, trough beds, gypsum veins and tangential beds (mainly in sediments). The main deposition environments are alluvial, fluvial and shallow lacustrine. Kibuku area is a potential area for hydrocarbon exploration.
Les informations fournies dans la section « Synopsis » peuvent faire référence à une autre édition de ce titre.
Kibuku area is located within Semlik sub basin, the southern part of the Albertine Graben in the western branch of the East Africa rift system. The rift flanks are underlined by basement rocks such as gneisses, quartzite, amphibolite, schist, and granitic-gneisses. Kibuku area is further divided into six formations namely Kisegi, Kasande, Kakara, Oluka, Nyaburogo and Katorogo, from oldest to youngest respectively. To delineate deposition environment and hydrocarbon potential; geologic mapping, grain size analysis, palaeocurrent analysis and sedimentologic logging.The main Syn rift Lithology encountered include clays, sands, silts, iron bands, pebbles, and conglomerates while Pre-rift Lithology includes schist, granitic-gneisses, mafic intrusions, amphibolite, gneisses and quartz veins. The structures included joints, faults, foliation (mainly in metamorphic rocks) and laminations, mega-ripple marks, tabular beds, trough beds, gypsum veins and tangential beds (mainly in sediments). The main deposition environments are alluvial, fluvial and shallow lacustrine. Kibuku area is a potential area for hydrocarbon exploration.
Patrick Mugwano is a research student at Pan African University Institute of Life and Earth Science in University of Ibadan, Jacob Mutua is a research student at Pan African University Institute of Life and Earth Science in University of Ibadan, Dr. Kevin Aanyu is a senior lecturer at Makerere University.
Les informations fournies dans la section « A propos du livre » peuvent faire référence à une autre édition de ce titre.
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Taschenbuch. Etat : Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -Kibuku area is located within Semlik sub basin, the southern part of the Albertine Graben in the western branch of the East Africa rift system. The rift flanks are underlined by basement rocks such as gneisses, quartzite, amphibolite, schist, and granitic-gneisses. Kibuku area is further divided into six formations namely Kisegi, Kasande, Kakara, Oluka, Nyaburogo and Katorogo, from oldest to youngest respectively. To delineate deposition environment and hydrocarbon potential; geologic mapping, grain size analysis, palaeocurrent analysis and sedimentologic logging.The main Syn rift Lithology encountered include clays, sands, silts, iron bands, pebbles, and conglomerates while Pre-rift Lithology includes schist, granitic-gneisses, mafic intrusions, amphibolite, gneisses and quartz veins. The structures included joints, faults, foliation (mainly in metamorphic rocks) and laminations, mega-ripple marks, tabular beds, trough beds, gypsum veins and tangential beds (mainly in sediments). The main deposition environments are alluvial, fluvial and shallow lacustrine. Kibuku area is a potential area for hydrocarbon exploration. 60 pp. Englisch. N° de réf. du vendeur 9783330337015
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Etat : New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Autor/Autorin: Mugwano PatrickPatrick Mugwano is a research student at Pan African University Institute of Life and Earth Science in University of Ibadan, Jacob Mutua is a research student at Pan African University Institute of Life and Earth Sc. N° de réf. du vendeur 385708580
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Taschenbuch. Etat : Neu. nach der Bestellung gedruckt Neuware - Printed after ordering - Kibuku area is located within Semlik sub basin, the southern part of the Albertine Graben in the western branch of the East Africa rift system. The rift flanks are underlined by basement rocks such as gneisses, quartzite, amphibolite, schist, and granitic-gneisses. Kibuku area is further divided into six formations namely Kisegi, Kasande, Kakara, Oluka, Nyaburogo and Katorogo, from oldest to youngest respectively. To delineate deposition environment and hydrocarbon potential; geologic mapping, grain size analysis, palaeocurrent analysis and sedimentologic logging.The main Syn rift Lithology encountered include clays, sands, silts, iron bands, pebbles, and conglomerates while Pre-rift Lithology includes schist, granitic-gneisses, mafic intrusions, amphibolite, gneisses and quartz veins. The structures included joints, faults, foliation (mainly in metamorphic rocks) and laminations, mega-ripple marks, tabular beds, trough beds, gypsum veins and tangential beds (mainly in sediments). The main deposition environments are alluvial, fluvial and shallow lacustrine. Kibuku area is a potential area for hydrocarbon exploration. N° de réf. du vendeur 9783330337015
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Taschenbuch. Etat : Neu. This item is printed on demand - Print on Demand Titel. Neuware -Kibuku area is located within Semlik sub basin, the southern part of the Albertine Graben in the western branch of the East Africa rift system. The rift flanks are underlined by basement rocks such as gneisses, quartzite, amphibolite, schist, and granitic-gneisses. Kibuku area is further divided into six formations namely Kisegi, Kasande, Kakara, Oluka, Nyaburogo and Katorogo, from oldest to youngest respectively. To delineate deposition environment and hydrocarbon potential; geologic mapping, grain size analysis, palaeocurrent analysis and sedimentologic logging.The main Syn rift Lithology encountered include clays, sands, silts, iron bands, pebbles, and conglomerates while Pre-rift Lithology includes schist, granitic-gneisses, mafic intrusions, amphibolite, gneisses and quartz veins. The structures included joints, faults, foliation (mainly in metamorphic rocks) and laminations, mega-ripple marks, tabular beds, trough beds, gypsum veins and tangential beds (mainly in sediments). The main deposition environments are alluvial, fluvial and shallow lacustrine. Kibuku area is a potential area for hydrocarbon exploration.VDM Verlag, Dudweiler Landstraße 99, 66123 Saarbrücken 60 pp. Englisch. N° de réf. du vendeur 9783330337015
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Taschenbuch. Etat : Neu. Depositional Environment and Hydrocarbon Potential of Kibuku Area | Patrick Mugwano | Taschenbuch | 60 S. | Englisch | 2017 | LAP LAMBERT Academic Publishing | EAN 9783330337015 | Verantwortliche Person für die EU: preigu GmbH & Co. KG, Lengericher Landstr. 19, 49078 Osnabrück, mail[at]preigu[dot]de | Anbieter: preigu. N° de réf. du vendeur 110657300
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