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Groundwater salinity influenced by Holocene seawater trapped in incised valleys in the Red River delta plain

Published on: Monday 24 April 2017

Groundwater salinity influenced by Holocene seawater trapped in incised valleys in the Red River delta plain Brackish to salty waters have been found in inland areas of delta aquifers. Geophysical data and modelling suggest that salty groundwater in the Red River delta originates from trapped seawater contained in underlying Holocene marine deposits.



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