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- W128839062 abstract "Flank margin caves form in the diffuse flow field of the distal margin of the freshwater lens on carbonate islands and coasts. Dissolution is governed by superposition of mixing zones at the top and bottom of the lens. Flow velocities in the lens margins and organic decay at the lens boundaries enhance dissolution. These caves grow from isolated initiation points in the lens into chambers that amalgamate to form complex, vertically restricted, globular-chamber complexes. The caves and their deposits accurately represent sea-level position and paleoclimate but must be successfully differentiated from sea caves and other pseudokarst features." @default.
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- W128839062 date "2013-01-01" @default.
- W128839062 modified "2023-09-23" @default.
- W128839062 title "6.29 Flank Margin Caves in Carbonate Islands and the Effects of Sea Level" @default.
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- W128839062 doi "https://doi.org/10.1016/b978-0-12-374739-6.00131-7" @default.
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