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Geologická a petrofyzikální charakteristika písčitého souvrství HAWAZ v ropném poli "H" na ložisku v pánvi Murzuq, JZ Libye
dc.contributor.advisorKobr, Miroslav
dc.creatorSherif, Yousef M.A.
dc.date.accessioned2019-05-03T14:46:49Z
dc.date.available2019-05-03T14:46:49Z
dc.date.issued2008
dc.identifier.urihttp://hdl.handle.net/20.500.11956/14003
dc.description.abstractThere are several basins with oil productive formations on the North African Platform. The Murzuq basin is one of them; it is situated in the south- west part of Libya and the northern portions of Niger, representing an intracratonic sag basin. It was initiated during the Palaeozoic Pan-African orogine. The deposition of the basin started with basal barren conglomerates of Hassaouna Formation unconformably overlying the Precambrian basement and being unconformably overlained by productive Hawaz Formation. The top of the Hawaz Formation is strictly demarcated by radioactive shales (lower Silurian Tanezzuft shales). The contact between top of the sedimental cycle of upper fluvial delta to shallow marine sea deposits and Silurian marine pelagic sediments documents an important palaeoclimatic change in sedimentary environment owing to Caledonian Unconformity. Silurian pelagic marine sediments represent an extensive marine flooding in all North-African Platform area. This flooding event of sea level rise was caused by melting and dissolving of the glacial material on the surrounding mountainous area during Caledonian unconformity, while this mountainous area transformed in peneplane. The present study is based on slabbed cores, core samples, and thin section; photographic of cores, conventional core...en_US
dc.description.abstractThere are several basins with oil productive formations on the North African Platform. The Murzuq basin is one of them; it is situated in the south- west part of Libya and the northern portions of Niger, representing an intracratonic sag basin. It was initiated during the Palaeozoic Pan-African orogine. The deposition of the basin started with basal barren conglomerates of Hassaouna Formation unconformably overlying the Precambrian basement and being unconformably overlained by productive Hawaz Formation. The top of the Hawaz Formation is strictly demarcated by radioactive shales (lower Silurian Tanezzuft shales). The contact between top of the sedimental cycle of upper fluvial delta to shallow marine sea deposits and Silurian marine pelagic sediments documents an important palaeoclimatic change in sedimentary environment owing to Caledonian Unconformity. Silurian pelagic marine sediments represent an extensive marine flooding in all North-African Platform area. This flooding event of sea level rise was caused by melting and dissolving of the glacial material on the surrounding mountainous area during Caledonian unconformity, while this mountainous area transformed in peneplane. The present study is based on slabbed cores, core samples, and thin section; photographic of cores, conventional core...cs_CZ
dc.languageEnglishcs_CZ
dc.language.isoen_US
dc.publisherUniverzita Karlova, Přírodovědecká fakultacs_CZ
dc.titleGeological and Petrophysical Characterization of Hawaz Sandstones Reservoir in ‚H' Oil Field, Murzuq Basin, SW Libyaen_US
dc.typedizertační prácecs_CZ
dcterms.created2008
dcterms.dateAccepted2008-03-19
dc.description.departmentInstitute of Hydrogeology, Engineering Geology and Applied Geophysicsen_US
dc.description.departmentÚstav hydrogeologie, inž. geologie a užité geofyzikycs_CZ
dc.description.facultyFaculty of Scienceen_US
dc.description.facultyPřírodovědecká fakultacs_CZ
dc.identifier.repId112609
dc.title.translatedGeologická a petrofyzikální charakteristika písčitého souvrství HAWAZ v ropném poli "H" na ložisku v pánvi Murzuq, JZ Libyecs_CZ
dc.contributor.refereeČepek, Petr
dc.contributor.refereeLukeš, Jiří
dc.identifier.aleph002132145
thesis.degree.namePh.D.
thesis.degree.leveldoktorskécs_CZ
thesis.degree.disciplineAplikovaná geologie se zaměřenímics_CZ
thesis.degree.disciplineApplied Geology with Specializationsen_US
thesis.degree.programAplikovaná geologiecs_CZ
thesis.degree.programApplied Geologyen_US
uk.faculty-name.csPřírodovědecká fakultacs_CZ
uk.faculty-name.enFaculty of Scienceen_US
uk.faculty-abbr.csPřFcs_CZ
uk.degree-discipline.csAplikovaná geologie se zaměřenímics_CZ
uk.degree-discipline.enApplied Geology with Specializationsen_US
uk.degree-program.csAplikovaná geologiecs_CZ
uk.degree-program.enApplied Geologyen_US
thesis.grade.csProspěl/acs_CZ
thesis.grade.enPassen_US
uk.abstract.csThere are several basins with oil productive formations on the North African Platform. The Murzuq basin is one of them; it is situated in the south- west part of Libya and the northern portions of Niger, representing an intracratonic sag basin. It was initiated during the Palaeozoic Pan-African orogine. The deposition of the basin started with basal barren conglomerates of Hassaouna Formation unconformably overlying the Precambrian basement and being unconformably overlained by productive Hawaz Formation. The top of the Hawaz Formation is strictly demarcated by radioactive shales (lower Silurian Tanezzuft shales). The contact between top of the sedimental cycle of upper fluvial delta to shallow marine sea deposits and Silurian marine pelagic sediments documents an important palaeoclimatic change in sedimentary environment owing to Caledonian Unconformity. Silurian pelagic marine sediments represent an extensive marine flooding in all North-African Platform area. This flooding event of sea level rise was caused by melting and dissolving of the glacial material on the surrounding mountainous area during Caledonian unconformity, while this mountainous area transformed in peneplane. The present study is based on slabbed cores, core samples, and thin section; photographic of cores, conventional core...cs_CZ
uk.abstract.enThere are several basins with oil productive formations on the North African Platform. The Murzuq basin is one of them; it is situated in the south- west part of Libya and the northern portions of Niger, representing an intracratonic sag basin. It was initiated during the Palaeozoic Pan-African orogine. The deposition of the basin started with basal barren conglomerates of Hassaouna Formation unconformably overlying the Precambrian basement and being unconformably overlained by productive Hawaz Formation. The top of the Hawaz Formation is strictly demarcated by radioactive shales (lower Silurian Tanezzuft shales). The contact between top of the sedimental cycle of upper fluvial delta to shallow marine sea deposits and Silurian marine pelagic sediments documents an important palaeoclimatic change in sedimentary environment owing to Caledonian Unconformity. Silurian pelagic marine sediments represent an extensive marine flooding in all North-African Platform area. This flooding event of sea level rise was caused by melting and dissolving of the glacial material on the surrounding mountainous area during Caledonian unconformity, while this mountainous area transformed in peneplane. The present study is based on slabbed cores, core samples, and thin section; photographic of cores, conventional core...en_US
uk.file-availabilityV
uk.publication.placePrahacs_CZ
uk.grantorUniverzita Karlova, Přírodovědecká fakulta, Ústav hydrogeologie, inž. geologie a užité geofyzikycs_CZ
thesis.grade.codeP


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