GEOLOGICAL CHARACTERISTICS OF TEHRAN AQUIFER
The alluvial deposits of Tehran is composed of up to 1100 m and is divided into five parts: The first part (~500 m) has been denominated as first member of Hezardareh Formation and has been formed of hard conglomerate of Upper Pliocene age. This part has many few porosity, high erodibility of pebble...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
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Associação Brasileira de Águas Subterrâneas
2002-07-01
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| Series: | Revista Águas Subterrâneas |
| Subjects: | |
| Online Access: | https://aguassubterraneas.abas.org/asubterraneas/article/view/22565 |