Geological Exploration Work in The Miocene-Quaternary Sediments in License Areas in The Deep Sea Zone of The Western Part of The Delta Nile (Egypt)тезисы доклада
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Дата последнего поиска статьи во внешних источниках: 4 марта 2022 г.
Аннотация:The Analysis of gathered data in the Western Delta of Deep-Sea field such as seismic lines of 3D cubes and well logging data, allows us to divide the thickness pattern of the basin into two mega sequences: Pre and Post Messinian complexes; as a result, sea level underwent 6 cycles of transgressive/regressive sedimentation during the evolution of the Miocene-Pleistocene period. Each multiform or individual hidden buried meandering-type channel has been found within the lenticular form. These channels can be traced, as they appear as bright spots in seismic profiles and are approved for additional inspection to discover hydrocarbons, Especially Pre/Messinian complex, which is considered for possible exploration to find more possible targets and prospects. The interpreted large tectonic structure is the offshore Nile Delta anticlinal uplift, which is a characteristic overlap that can create a competent and appropriate structural hydrocarbon trap in the sandy siliceous-detrital formations in the Western Delta of