Terrestrische Sedimente der Intermontanbecken im Iran |
| |
| Authors: | Dr-Ing Mehdi Nadji |
| |
| Institution: | 1. Karimkhan Zand Ave. 54/5, Teheran, Iran
|
| |
| Abstract: | Noteworthy facts about terrestrial deposits which fill the Internal Basins in Iran have been studied mainly in the last decade. Hydrogeological investigations in more than 100 alluvial basins have been most informative for essential knowledge about the structure of and sedimentation in the extensive plains. The thickness of the alluvial deposits ranges in different amount. Its known maximum, above 500 m, is located in the area between Teheran and Karaj. By the example of Varamin Plain it is shown that the sedimentation has an unequivocal dependence on the recent drainage pattern. The trace of“Water veins” is very important for exploration of ground water. The“Veins” are ancient washes filled up with outwashed gravels which are covered later with younger fine grained materials. The occurrence of these highly permeable deposits can be found by means of sedimentological investigations. |
| |
| Keywords: | |
| 本文献已被 SpringerLink 等数据库收录！ |
|
