Researching of relationship between sequence stratigraphy, lithofacies and aquifer and aquifuge of Quaternary sediments in Thai Binh and Nam Dinh area
DOI:
https://doi.org/10.5281/zenodo.13853740Từ khóa:
Stratigraphy, Pleistocen, SedimentTóm tắt
The Pleistocene aquifer in Thai Binh and Nam Dinh area is related to 5 riverbed sand facies complexes belonging to the lowstand systems tract and 5 highstand river mouth sandy bar sand facies complex with ages ranging from Early Pleistocene late late Pleistocene: (1) (SaLSTQ11); (2) (SaLSTQ12a+SamHSTQ11); (3) (SaLSTQ12b+SamHSTQ12a); (4) (SaLSTQ13a+SamHSTQ12b; (5)(SaSTQ13b+SamHSTQ13a). Overlaying these 5 aquifers are 5 aquifuges including 5 transgessive systems tract shallow marine-bay mud facies complexes: (1) MmTSTQ11; (2) MmTSTQ12a; (3) MmTSTQ12b; (4) MmTSTQ13a; (5) MmTSTQ21-2. The process salinization of has
been occurring in the Pleistocene aquifer in Nam Dinh and Thai Binh areas due to the permeation of meteorological water through shallow sea-bay marine mud facies complexes that act as aquitard layer. Residual salt water fro
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