STUDY OF FRACTURED STRUCTURE OF SARAB GHANBAR AT SOUTH OF KERMANSHAH CITY USING GPR METHOD

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.

OVEYSI MOUAKHAR M.

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

Journal Paper

Paper Information

Journal: IRANIAN JOURNAL OF GEOPHYSICS Year:2008 | Volume:1 | Issue:1 Page(s): 81-89

Download Full-Text

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

Persian Verion

View:

803

Download:

Cites:

Information Journal Paper

Title

STUDY OF FRACTURED STRUCTURE OF SARAB GHANBAR AT SOUTH OF KERMANSHAH CITY USING GPR METHOD

Author(s)

OVEYSI MOUAKHAR M. | Issue Writer Certificate

Keywords

RADAR METHODQ3

SHALLOW METHODQ3

RADIOLARITESQ3

FRACTURESQ3

ANTICLINEQ3

Abstract

RADAR METHOD (GPR) is one of the electromagnetic methods to detect shallow depth of underground layers. Sarab E Ghanbar region which is situated at south of Kermanshah city is at thrusted Zagros region. At this region limestone with different ages are adjacent to RADIOLARITES sediments. Due to fractured Limestone and low permeability of RADIOLARITES, study of RADIOLARITES is important as the latter acts as a dam to water flow from limestone. 100MHZ unshielded antenna has been used to a small part of RADIOLARITES to detect fractured and deformed layers. Depth of penetration of radar waves is lm and their velocity is 0.069m/ns. Radargrams show the main fracture at 8m from the first point of the measurements. Deformed layers are located at different horizontal distances at maximum depth of 1.5m. Some radargrams show an ANTICLINE at 22m which is in agreement with field observation.

Cites

No record.

References

No record.

Cite

APA: Copy

OVEYSI MOUAKHAR, M.. (2008). STUDY OF FRACTURED STRUCTURE OF SARAB GHANBAR AT SOUTH OF KERMANSHAH CITY USING GPR METHOD. IRANIAN JOURNAL OF GEOPHYSICS, 1(1), 81-89. SID. https://sid.ir/paper/133807/en

Vancouver: Copy

OVEYSI MOUAKHAR M.. STUDY OF FRACTURED STRUCTURE OF SARAB GHANBAR AT SOUTH OF KERMANSHAH CITY USING GPR METHOD. IRANIAN JOURNAL OF GEOPHYSICS[Internet]. 2008;1(1):81-89. Available from: https://sid.ir/paper/133807/en

IEEE: Copy

M. OVEYSI MOUAKHAR, “STUDY OF FRACTURED STRUCTURE OF SARAB GHANBAR AT SOUTH OF KERMANSHAH CITY USING GPR METHOD,” IRANIAN JOURNAL OF GEOPHYSICS, vol. 1, no. 1, pp. 81–89, 2008, [Online]. Available: https://sid.ir/paper/133807/en

Related Journal Papers