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- W2110131138 abstract "Facies analyses of Pleistocene deposits from southern coastal Tanzania (Lindi District) document that sediments formed in a wetland evolving on a coastal terrace in the Lindi Fracture Zone foreland. The exposed succession shows a marked sedimentary change from tidal to terrestrial facies. 14 C analyses on gastropod shells indicate the emergence of the Lindi coast at ∼ 44 14 C ka BP. Emergence and subsequent elevation of terraces to 21 m above present-day sea level was linked to the falling eustatic sea level prior to the last glacial maximum, and to a periodic elevation due to extensional tectonic episodes in the eastern branch of the East African Rift System (EARS). Since ∼ 44 14 C ka BP tectonic uplift at the coast was 80-110 m, comparable to that in the extreme uplift areas of the EARS." @default.
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- W2110131138 date "2010-01-01" @default.
- W2110131138 modified "2023-09-25" @default.
- W2110131138 title "Sedimentary Evolution of a Late Pleistocene Wetland Indicating Extreme Coastal Uplift in Southern Tanzania" @default.
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- W2110131138 doi "https://doi.org/10.1016/j.yqres.2009.09.004" @default.
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