GEOMORPHOLOGY OF MEYGHAN BASIN THE SURVEY OF GEOMORPHOLOGICAL LANDFORMS AND RANGE OF THEIR DEVELOPMENT

Q: How can I download an article?

To download an article from SID, first log in to the site, search for the article title, and click on the 'Download Article' option.

Q: How can I download an ISI article?

To download an ISI article on SID, enter the keyword or article title in the search bar, view the relevant results, click on the desired article, and select the 'Download Article' option.

Q: How can I access the SID database?

To access the SID database, visit SID.ir, create an account, and log in to access scientific resources.

Q: Is downloading articles from SID free?

Some articles on SID are available for free, while others require payment. Details are specified on the article's page.

GHANAVATI E.A.; MIRZAKHANI B.; ASGARI A.

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Journal Paper

Paper Information

Journal: JOURNAL OF PHYSICAL GEOGRAPHY Year:2012 | Volume:5 | Issue:17 Page(s): 1-12

Download Full-Text

Persian Verion

View:

782

Download:

Cites:

Information Journal Paper

Title

GEOMORPHOLOGY OF MEYGHAN BASIN THE SURVEY OF GEOMORPHOLOGICAL LANDFORMS AND RANGE OF THEIR DEVELOPMENT

Author(s)

GHANAVATI E.A. | MIRZAKHANI B. | ASGARI A. | Issue Writer Certificate

Keywords

PLAYAQ2

MEYGHANQ2

GEOMORPHOLOGYQ2

CATCHMENTQ2

GISQ2

Abstract

There are several lakes in the center of the Iran that are the end basin in dry zone. These are called PLAYA lakes. Since the PLAYA is a part of larger system, that called the CATCHMENT, the study of PLAYAs also require to careful consideration of the CATCHMENT that ends to them. This research with aim of geomorphological evaluate of MEYGHAN basin using 1:50000 maps, ETM images of the Landsat satellite, IRS P6 image and geological map and field observations have been made. Arc GIS 9.3 and ERDAS 9.1 softwares were used for geomorphologic mapping. MEYGHAN lake has been formed in a synclinal subsidence, and the main faults of the Tabarte and Talkhab pass through it and it has been divided into smaller units include of the volcanic belt of the Orumiye- Dokhtar, Haftad Ghole and Sanandaj - Sirjan zone. Results of the study suggest the existence of karst forms as caves, Nebkas, glacis, alluvial fans and another form.

Cites

No record.

References

Cite

APA: Copy

GHANAVATI, E.A., MIRZAKHANI, B., & ASGARI, A.. (2012). GEOMORPHOLOGY OF MEYGHAN BASIN THE SURVEY OF GEOMORPHOLOGICAL LANDFORMS AND RANGE OF THEIR DEVELOPMENT. JOURNAL OF PHYSICAL GEOGRAPHY, 5(17), 1-12. SID. https://sid.ir/paper/184990/en

Vancouver: Copy

GHANAVATI E.A., MIRZAKHANI B., ASGARI A.. GEOMORPHOLOGY OF MEYGHAN BASIN THE SURVEY OF GEOMORPHOLOGICAL LANDFORMS AND RANGE OF THEIR DEVELOPMENT. JOURNAL OF PHYSICAL GEOGRAPHY[Internet]. 2012;5(17):1-12. Available from: https://sid.ir/paper/184990/en

IEEE: Copy

E.A. GHANAVATI, B. MIRZAKHANI, and A. ASGARI, “GEOMORPHOLOGY OF MEYGHAN BASIN THE SURVEY OF GEOMORPHOLOGICAL LANDFORMS AND RANGE OF THEIR DEVELOPMENT,” JOURNAL OF PHYSICAL GEOGRAPHY, vol. 5, no. 17, pp. 1–12, 2012, [Online]. Available: https://sid.ir/paper/184990/en

Related Journal Papers