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Effect of groundwater level changes on geodetic observations: case study of Tehran basin, Iran
نويسندهگان:
yahya Djamour - Geodesy and surveying Dept., National Cartographic Center , Tehran
R.Bayer - Laboratoire Dynamique de la Lithosphere,University of Montpellier II, Montpellier France.
خلاصه مقاله:
The aquifer system of Tehran is located to the south side of Central Alborz. This basin is built on a Plio-Quaternary unconsolidated sediments about 50km larg from the north to the south (FIG-1). The formation of this foreland basin is associated with Alborz mountain structure. This basin is affected by numerous active thrusts in Plio-Quaternary time. The Tehran aquifer is charged mainly by Karaj and Kan alluvialcones.
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