A comparison between karst development in two main zones of Iran: case study—Keyno anticline (Zagros Range) and Shotori anticline (Central Iran)-Reference-Cited by-同舟云学术

A comparison between karst development in two main zones of Iran: case study—Keyno anticline (Zagros Range) and Shotori anticline (Central Iran)

Published:2015-06-03 Issue:12 Volume:8 Page:10833-10844
ISSN:1866-7511
Container-title:Arabian Journal of Geosciences
language:en
Short-container-title:Arab J Geosci

Author:

Chitsazan Manouchehr,Karimi Vardanjani Hossein,Karimi Haji,Charchi Abbas

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences,General Environmental Science

Link

http://link.springer.com/content/pdf/10.1007/s12517-015-1961-x.pdf

Reference10 articles.

1. Aghanabati A (2004) Geology of Iran. Geological Survey of Iran, Tehran

2. Ashjari J, Raeisi E (2006) Anticlinal structure influences on regional flow, Zagross, Iran. J caves and karst stud 68(3):118–129

3. Doctor DH, Alexander EC Jr (2005) Interpretation of water chemistry and stable isotope data from a Karst aquifer according to flow regimes identified through hydrograph recession analysis. In: Kuniansky EL (ed) U.S. Geological Survey Karst Interest Group Proceedings, Rapid City, South Dakota, September 12–15, 2005: U.S. Geological Survey Scientific Investigations Report 2005–5160, p 82–92

4. Ford DC, Williams PW (2007) Karst hydrogeology and geomorphology. John Wiley & Sons Ltd, The Atrium, Southern Gate, Chichester

5. Hoetzl H (1995) Groundwater recharge in an arid karst area (Saudi Arabia), Application of Tracers in Arid Zone Hydrology (Proceedings of the Vienna Symposium, August 1994). IAHS Publ. no. 232

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