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- W26415071 abstract "The consistency of many of the 210Pb profiles implies that: • The glacial-marine processes that supplied, transported and deposited sediment in these sub-polar and polar fjords have not varied markedly. • This contrasts with other glacial-marine systems in warmer regions such as SE Alaska, where sedimentation in the fjords from calving temperate glaciers tends to vary significantly, and where the accumulation tends to slow as the calving front recedes rapidly from the core location." @default.
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- W26415071 date "2007-12-01" @default.
- W26415071 modified "2023-10-17" @default.
- W26415071 title "210-Pb Study of Fjord Sedimentation Rates in the South Shetland Islands and Antarctic Peninsula" @default.
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