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Karistineos, N.; Ioakim, C. |
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Title |
Palaeoenvironmental and palaeoclimatic evolution of the serres basin (N. Greece) during the miocene |
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Year |
1989 |
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Palaeogeography, Palaeoclimatology, Palaeoecology |
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70 |
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1-3 |
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275-285 |
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Abstract |
The palaeoenvironmental and palaeoclimatic evolution of the Serres basin from the end of mid-Miocene to the end of the Miocene is examined. Lignites were deposited over a thick sequence of conglomerates and sands. Fossils found in the lignites indicate a lacustrine environment with tropical-subtropical climatic conditions. The climate became progressively drier and only small lakes were reserved during the Messinian salinity crisis. Deposition of lake sediments finally ended with the world-wide Pliocene marine transgression. A correlation of the Serres basin with other lacustrine basins in the Aegean area is attempted. |
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Elsevier |
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0031-0182 |
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THL @ christoph.kuells @ Karistineos1989 |
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28 |
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Author |
Tziritis, E. |
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Title |
Groundwater and soil geochemistry of the Eastern Kopaida region (Beotia, central Greece) |
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Journal Article |
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2009 |
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Open Geosciences |
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1 |
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2 |
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219-226 |
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THL @ luqianxue.zhang @ tziritis2009groundwater |
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65 |
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Seyedmohammadi*, J.; Esmaeelnejad, L.; Shabanpour, M. |
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Title |
Spatial variation modeling of groundwater electrical conductivity using geostatistics and GIS |
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Journal Article |
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2016 |
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Model. Earth Syst. Environ. |
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2 |
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169 |
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CUT @ phaedon.kyriakidis @ Seyedmohammadi2016 |
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164 |
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Edmunds, W.M. |
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Title |
Bromine geochemistry of british groundwaters |
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Journal Article |
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1996 |
Publication |
Mineralogical Magazine |
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60 |
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399 |
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275-284 |
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\textlessp\textgreater The concentrations of Br in potable groundwaters in the United Kingdom range from 60 to 340 µg 1 \textlesssup\textgreater-1\textless/sup\textgreater . The occurrence of Br is described in terms of the Br/Cl weight ratio which enables small changes in bromide concentrations to be assessed in terms of salinity. Median values of Br/Cl in groundwaters range from 2.60 to 5.15 × 10 \textlesssup\textgreater−3\textless/sup\textgreater compared with a sea water ratio of 3.47× 10 \textlesssup\textgreater−3\textless/sup\textgreater . In recent shallow groundwaters the Br/Cl ratio is rather variable in response to a range of natural and anthropogenic inputs (marine and industrial aerosols, industrial and agricultural chemicals including road salt). Some slight enrichment in Br/Cl also occurs naturally during infiltration as a result of biogeochemical processes. \textless/p\textgreater |
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0026-461x |
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THL @ christoph.kuells @ Edmunds1996 |
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20 |
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Marengo*, E.; Gennaro, M.C.; Robotti, E.; Maiocchi, A.; Pavese, G.; Indaco, A.; Rainero, A. |
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Statistical analysis of ground water distribution in Alessandria Province (Piedmont—Italy) |
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2008 |
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Microchem. J. |
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88 |
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167-177 |
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CUT @ phaedon.kyriakidis @ Marengo2008 |
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134 |
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