DETERMINATION OF DESERT AREAS OF HORMOZGAN PROVINCE FROM GEOLOGICAL ASPECT

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.

CHOUPANI S.; KHOSROUSHAHI MOHAMMAD; GHOLAMPOUR M.; MIRAKHOURLOU KH.

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

Journal Paper

Paper Information

Journal: IRANIAN JOURNAL OF RANGE AND DESERT RESEARCH Year:2006 | Volume:13 | Issue:1 (22) Page(s): 17-26

Download Full-Text

Persian Verion

View:

1,217

Download:

Cites:

Information Journal Paper

Title

DETERMINATION OF DESERT AREAS OF HORMOZGAN PROVINCE FROM GEOLOGICAL ASPECT

Author(s)

CHOUPANI S. | KHOSROUSHAHI MOHAMMAD | GHOLAMPOUR M. | MIRAKHOURLOU KH. | Issue Writer Certificate

Keywords

HORMOZGAN PROVINCEQ3

EVAPO FORMATIONQ3

QUATERNARY FORMATIONQ3

PRIMARY DESERTQ2

SECONDARY DESERTQ2

Abstract

The country of Iran is situated in an arid and semi-arid zone, with an average precipitation of about 250 mm per year. HORMOZGAN PROVINCE in southern Iran, is one of the most arid parts of Iran with an average annual rainfall of only 170mm. The study area is located in the Zagros and Makran geological zones.. In the study area the oldest formations are of Palaeozoic age. Another characteristic of the Zagros zone are diapirs. Diapirs rise up from the deepest part of sedimentary rocks, and after cutting through the upper layers, they may appear at the surface, which seriously affect groundwater quality and land use.Desertification; in Iran has occurred from Neosene and Quaternary. Geological formation has important effect on salinisation and desertification. Thus, the geographical investigation of desert area is very important. This investigation is based on GIS method Applications, geological map (1:250000) and supported by, fieldwork. At the first, prepared and digitizing of geological maps by Ilwis program and was carefully checked and corrected where possible. The next step prepared evaporation formation and Quaternary maps and its overlying. Prepared cross map of Quaternary and Hydrographic network and determination of primary and SECONDARY DESERTs area. The final step was prepared a cross map of primary and SECONDARY DESERT area map and checked by fieldwork. To comparison between units of desert area map, can be result, more than 78 percent of study area is situated in the deserts area.

Cites

No record.

References

No record.

Cite

APA: Copy

CHOUPANI, S., KHOSROUSHAHI, MOHAMMAD, GHOLAMPOUR, M., & MIRAKHOURLOU, KH.. (2006). DETERMINATION OF DESERT AREAS OF HORMOZGAN PROVINCE FROM GEOLOGICAL ASPECT. IRANIAN JOURNAL OF RANGE AND DESERT RESEARCH, 13(1 (22)), 17-26. SID. https://sid.ir/paper/107002/en

Vancouver: Copy

CHOUPANI S., KHOSROUSHAHI MOHAMMAD, GHOLAMPOUR M., MIRAKHOURLOU KH.. DETERMINATION OF DESERT AREAS OF HORMOZGAN PROVINCE FROM GEOLOGICAL ASPECT. IRANIAN JOURNAL OF RANGE AND DESERT RESEARCH[Internet]. 2006;13(1 (22)):17-26. Available from: https://sid.ir/paper/107002/en

IEEE: Copy

S. CHOUPANI, MOHAMMAD KHOSROUSHAHI, M. GHOLAMPOUR, and KH. MIRAKHOURLOU, “DETERMINATION OF DESERT AREAS OF HORMOZGAN PROVINCE FROM GEOLOGICAL ASPECT,” IRANIAN JOURNAL OF RANGE AND DESERT RESEARCH, vol. 13, no. 1 (22), pp. 17–26, 2006, [Online]. Available: https://sid.ir/paper/107002/en

Related Journal Papers