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- W1968897795 abstract "Air-gun and 3.5-kHz seismic profiles from the eastern Aegean Sea off Turkey show that the continental shelf of outer Izmir and Candarli bays is formed by several superimposed deltaic sequences. During times of lowered sea level associated with late Quaternary glaciations, deltas prograded seaward more than 60 km from their present positions. Foreset progradation ceased with the rise of sea level in interglacial and post-glacial times and deltas were reestablished far inland in drowned river valleys. These major transgressions resulted in unconformities within the superimposed prograded delta sequences. The most recent three unconformities are correlated with the beginning of oxygen isotope stages 5, 3 and 1, and provide chronostratigraphic markers for a detailed analysis of sedimentation patterns in the late Quaternary. The coastal shelf and basins are subsiding at an average rate of about 1 m per 1000 years. This tectonic subsidence manifests itself as widespread normal block faulting which can be related to the pre-Miocene structural framework of the region." @default.
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- W1968897795 date "1987-01-01" @default.
- W1968897795 modified "2023-10-06" @default.
- W1968897795 title "Late Quaternary tectonic and sedimentary history of outer Izmir and Candarli bays, western Turkey" @default.
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- W1968897795 doi "https://doi.org/10.1016/0025-3227(87)90019-3" @default.
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