Geometry, Kinematic and dynamic analysis of Bamu fault zone in north of Shiraz, Zagros Folded Belt Zone

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.

Bandegani Ali; YASSAGHI ALI; ELIASSI MOHSEN

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

Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2021 | Volume:30 | Issue:118 Page(s): 215-224

Download Full-Text

Persian Verion

View:

398

Download:

Cites:

Information Journal Paper

Title

Geometry, Kinematic and dynamic analysis of Bamu fault zone in north of Shiraz, Zagros Folded Belt Zone

Author(s)

Bandegani Ali | YASSAGHI ALI | ELIASSI MOHSEN | Issue Writer Certificate

Keywords

Bamu fault zoneQ1

Zagros Folded belt zoneQ2

Fault kinematicsQ1

PaleostressQ2

Abstract

In this paper, the structural evolution of Bamu fault zone located in the Zagros Folded belt zone is presented as an example of northeast-trending fault zone in the Zagros, using the kinematic and dynamic analysis of accompanied structures. Based on structural and Paleostress analyzes two phases of shortening were determined as NE and NNE. In order to define the chronology of the deformation stages in the region, the relationship between fault structures and folds in the folded rock formations has been utilized. The result showed that the first compression stress trend in the area was NE that caused formation of the Bamu transverse Fault with left-lateral strike-slip mechanism and its accompanied structures. Since this stage of deformation has affected the Oligocene-early Miocene formations, more likely occurred at this time. During the next phase the shortening direction, due to change in the collision zone direction of the Arabian-central Iran in the Miocene-Pliocene, has changed to NNE which causes development of younger structures in the form of folding and reverse faulting in the fault zone. This shows that the NE-trending fault zones, like other major NW-faults, in Zagros affected by the change in the convergence of Zagros collision.

Cites

No record.

References

No record.

Cite

APA: Copy

Bandegani, Ali, YASSAGHI, ALI, & ELIASSI, MOHSEN. (2021). Geometry, Kinematic and dynamic analysis of Bamu fault zone in north of Shiraz, Zagros Folded Belt Zone. GEOSCIENCES, 30(118 ), 215-224. SID. https://sid.ir/paper/389393/en

Vancouver: Copy

Bandegani Ali, YASSAGHI ALI, ELIASSI MOHSEN. Geometry, Kinematic and dynamic analysis of Bamu fault zone in north of Shiraz, Zagros Folded Belt Zone. GEOSCIENCES[Internet]. 2021;30(118 ):215-224. Available from: https://sid.ir/paper/389393/en

IEEE: Copy

Ali Bandegani, ALI YASSAGHI, and MOHSEN ELIASSI, “Geometry, Kinematic and dynamic analysis of Bamu fault zone in north of Shiraz, Zagros Folded Belt Zone,” GEOSCIENCES, vol. 30, no. 118 , pp. 215–224, 2021, [Online]. Available: https://sid.ir/paper/389393/en

Related Journal Papers