SURVEY OF SANGBAST-SHANDIZ FAULT ZONE GROWTH AND GEOMORPHOLOGICAL RESULTS

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.

ZERAATKAR ALI KEIVAN; RAHIMI BEHNAM

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

Journal Paper

Paper Information

Journal: Journal of Geography and Regional Development Year:2013 | Volume:- | Issue:19 Page(s): 195-214

Download Full-Text

Persian Verion

View:

2,174

Download:

Cites:

Information Journal Paper

Title

SURVEY OF SANGBAST-SHANDIZ FAULT ZONE GROWTH AND GEOMORPHOLOGICAL RESULTS

Author(s)

ZERAATKAR ALI KEIVAN | RAHIMI BEHNAM | Issue Writer Certificate

Keywords

STRIKE-SLIP FAULT GROWTHQ2

GEOMORPHOLOGY OF FAULT ZONEQ2

BINALUD MOUNTAINSQ2

Abstract

The Sangbast-Shandiz fault zone, with a length of about 57 km, a width of moderately 2 km, and a NW-SE direction, is located about 15 km in the west of Mashhad city. That is one of the major faults in the BINALUD MOUNTAINS. Geomorphic evidences illustrate that the Sangbast-Shandiz fault zone has dextral strike- slip offsets with thrust activity. In this article, we investigated geomorphic features of faulting, by using remote sensing analysis of satellite images, digital elevation maps, and field work studies. These geomorphic attributes consist of a topographical distortion along the fault line on the surface and offsets or cutting in liner features as drainage systems like stream channels and liner eroding crests. In the results, we found out that increasing of fault slip quantity, increased elongation, widened the fault segments, and so joined pre-existing faults and segments and decreased fault steps. In addition, the southeast mid of Sangbast-Shandiz fault zone is releasing energy and seems to be in a growing state while the northwest mid is in a compressing stress state.

Cites

No record.

References

No record.

Cite

APA: Copy

ZERAATKAR, ALI KEIVAN, & RAHIMI, BEHNAM. (2013). SURVEY OF SANGBAST-SHANDIZ FAULT ZONE GROWTH AND GEOMORPHOLOGICAL RESULTS. JOURNAL OF GEOGRAPHY AND REGIONAL DEVELOPMENT, -(19), 195-214. SID. https://sid.ir/paper/99007/en

Vancouver: Copy

ZERAATKAR ALI KEIVAN, RAHIMI BEHNAM. SURVEY OF SANGBAST-SHANDIZ FAULT ZONE GROWTH AND GEOMORPHOLOGICAL RESULTS. JOURNAL OF GEOGRAPHY AND REGIONAL DEVELOPMENT[Internet]. 2013;-(19):195-214. Available from: https://sid.ir/paper/99007/en

IEEE: Copy

ALI KEIVAN ZERAATKAR, and BEHNAM RAHIMI, “SURVEY OF SANGBAST-SHANDIZ FAULT ZONE GROWTH AND GEOMORPHOLOGICAL RESULTS,” JOURNAL OF GEOGRAPHY AND REGIONAL DEVELOPMENT, vol. -, no. 19, pp. 195–214, 2013, [Online]. Available: https://sid.ir/paper/99007/en

Related Journal Papers