SEPARATION OF PALEOSTRESSES PHASES BASED ON HETEROGENEOUS FAULT-SLIP DATA IN THE CENTRAL PART OF DEHSHIR FAULT

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.

MOSHREFIFAR M.R.; ALAVI A.; MOHAJEL MOHAMMAD

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

Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2008 | Volume:18 | Issue:69 Page(s): 64-73

Download Full-Text

Persian Verion

View:

877

Download:

Cites:

Information Journal Paper

Title

SEPARATION OF PALEOSTRESSES PHASES BASED ON HETEROGENEOUS FAULT-SLIP DATA IN THE CENTRAL PART OF DEHSHIR FAULT

Author(s)

MOSHREFIFAR M.R. | ALAVI A. | MOHAJEL MOHAMMAD | Issue Writer Certificate

Keywords

STRIK-SLIP FAULTQ2

DEHSHIR FAULTQ3

PALESOSTRESSQ2

MULTIPLE INVERSE METHODQ3

Abstract

In this research, separation of paleostress phases in the central part of DEHSHIR FAULT is investigated based on the study heterogeneous fault-slip data and their related slickenside lineation’s. These data are measured from the Certaceous (Taft limestone), early Eocene (Kerman conglomerate) and Eocene (Volcanics) formations. The main criteria used here to identify sense of fault-slip are stratiographic separation, accretionary mineral steps, Riedel shears and tension gash. The existing faults iberegion of investigated often show two NE and NW trend in which the latter is usually dominant. Based on the study of heterogeneous fault-slip data and their related slickenside lineation’s and using the MULTIPLE INVERSE METHODs, at least two phases expected. These phases show that the axis of maximum principal stress, s1, is at NE trend and that of minimum principal s3 is, at NW trend. The location of s3 usually indicates that the strike-slip and reverse strike-slip faults mostly occur in the on lnaddition, the shape of the stress ellipsoid is prelate in the region.

Cites

STRUCTURAL EVIDENCE OF CHANGES IN TECTONIC REGIME FROM COMPRESSIONAL STRESS TO COMPRESSION-SHEAR STRESS IN SOUTHEAST OF THE GAVKHUNI (KHUSHAB REGION)

References

DETERMINATION OF STRESS STATE AND DIRECTION BY INVERSION OF FAULT-SLIP DATA IN THE SOUTHERN OF FLANK OF CENTRAL ALBORZ

Cite

APA: Copy

MOSHREFIFAR, M.R., ALAVI, A., & MOHAJEL, MOHAMMAD. (2008). SEPARATION OF PALEOSTRESSES PHASES BASED ON HETEROGENEOUS FAULT-SLIP DATA IN THE CENTRAL PART OF DEHSHIR FAULT. GEOSCIENCES, 18(69), 64-73. SID. https://sid.ir/paper/32457/en

Vancouver: Copy

MOSHREFIFAR M.R., ALAVI A., MOHAJEL MOHAMMAD. SEPARATION OF PALEOSTRESSES PHASES BASED ON HETEROGENEOUS FAULT-SLIP DATA IN THE CENTRAL PART OF DEHSHIR FAULT. GEOSCIENCES[Internet]. 2008;18(69):64-73. Available from: https://sid.ir/paper/32457/en

IEEE: Copy

M.R. MOSHREFIFAR, A. ALAVI, and MOHAMMAD MOHAJEL, “SEPARATION OF PALEOSTRESSES PHASES BASED ON HETEROGENEOUS FAULT-SLIP DATA IN THE CENTRAL PART OF DEHSHIR FAULT,” GEOSCIENCES, vol. 18, no. 69, pp. 64–73, 2008, [Online]. Available: https://sid.ir/paper/32457/en

Related Journal Papers