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- W2002606951 abstract "The existing stratigraphic framework of theEocene-Miocene in the study area (sector 5) shows limited temporal stratigraphicand structural resolution. Using this framework, it is difficult to unravel theinfluence of possible local tectonic movements and eustatic sea level changeson sedimentation. The precise influence of the onset of the possible Late Eocene-EarlyOligocene orogenic phase, which caused inversion and uplift in the study area(sector 5), is also dubious as a result of the limited data. To improve thecorrelations and recognition of the Eocene to Oligocene successions in the areain question (from sector 1 to sector 8), a new stratigraphic interpretation,based on correlated lithostratigraphic columns from different outcrops, ispresented. The changes in sedimentation and tectonic events in the study areacan be correlated to time-equivalent sea level changes and tectonic uplift inAl Jabal Al Akhdar area, which suggests that the processes causing the sedimento/structuralactivity are of regional importance." @default.
- W2002606951 created "2016-06-24" @default.
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- W2002606951 date "2013-01-01" @default.
- W2002606951 modified "2023-09-25" @default.
- W2002606951 title "Possible Geological Reason for the Missing of the Oligocene Section in Sector (5) and Its Vicinity, Deryanah-Al Abyar Area, Al Jabal Al Akhdar, NE Libya" @default.
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- W2002606951 doi "https://doi.org/10.4236/ojg.2013.34037" @default.
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