ASSESSMENT OF THE EFFECT OF FRACTURES ON THE OCCURRENCE OF SPRINGS IN SARDASHT AND SHAYOUN AREA IN KHUZESTAN PROVINCE

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.

KALANTARI N.A.; KARAMI FARD M.; CHARCHI A.

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

Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2007 | Volume:16 | Issue:62 Page(s): 62-71

Download Full-Text

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

Persian Verion

View:

1,061

Download:

Cites:

Information Journal Paper

Title

ASSESSMENT OF THE EFFECT OF FRACTURES ON THE OCCURRENCE OF SPRINGS IN SARDASHT AND SHAYOUN AREA IN KHUZESTAN PROVINCE

Author(s)

KALANTARI N.A. | KARAMI FARD M. | CHARCHI A. | Issue Writer Certificate

Keywords

FRACTURESQ3

STRUCTURAL FACTORSQ3

SPRINGSQ3

SAND STONEQ2

DEZFUL EMBAYMENTQ3

Abstract

The Sardasht and Shayoun area in the north of DEZFUL EMBAYMENT structure and on the southwest of Zagros structural belt is affected by shear zone pattern of Balarud. This watershed occupies an area of about 1042 km2 and encompasses parts of Dez, Shirinab and Sardashat watersheds. The purpose of this investigation is the assessment of STRUCTURAL FACTORS (specifically FRACTURES) on sandstone permeability and spring occurrence in the study area. In this investigation, geology and structural geology including folding, faulting and fracture studies were carried out. For fracture examination, joint data collections from eleven stations were analyzed and the collected data taken into account to prepare the structural map of the area. The iso-density fracture map indicates more permeable zones. It is also evident from the map that SPRINGS are mostly occurring in dense fracture zones of the area. The position of the SPRINGS, their structural and qualitative characteristics were assessed, and found that SPRINGS with more discharge, showed more temperature fluctuation in wet and dry seasons.

Cites

ASSESSMENT OF FACTORS INFLUENCING OCCURRENCE OF IZEH PLAIN WATERSHED SPRINGS

References

No record.

Cite

APA: Copy

KALANTARI, N.A., KARAMI FARD, M., & CHARCHI, A.. (2007). ASSESSMENT OF THE EFFECT OF FRACTURES ON THE OCCURRENCE OF SPRINGS IN SARDASHT AND SHAYOUN AREA IN KHUZESTAN PROVINCE. GEOSCIENCES, 16(62), 62-71. SID. https://sid.ir/paper/31929/en

Vancouver: Copy

KALANTARI N.A., KARAMI FARD M., CHARCHI A.. ASSESSMENT OF THE EFFECT OF FRACTURES ON THE OCCURRENCE OF SPRINGS IN SARDASHT AND SHAYOUN AREA IN KHUZESTAN PROVINCE. GEOSCIENCES[Internet]. 2007;16(62):62-71. Available from: https://sid.ir/paper/31929/en

IEEE: Copy

N.A. KALANTARI, M. KARAMI FARD, and A. CHARCHI, “ASSESSMENT OF THE EFFECT OF FRACTURES ON THE OCCURRENCE OF SPRINGS IN SARDASHT AND SHAYOUN AREA IN KHUZESTAN PROVINCE,” GEOSCIENCES, vol. 16, no. 62, pp. 62–71, 2007, [Online]. Available: https://sid.ir/paper/31929/en

Related Journal Papers