STRUCTURAL ANALYSIS OF DOWGONBADAN REGION, ZAGROS FOLD THRUST BELT, AN INSTANCE OF FRONTAL AND LATERAL RAMP

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.

NARIMANI H.; YASSAGHI A.; HASSAN GOODARZI M.GH.

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

Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2012 | Volume:21 | Issue:82 Page(s): 53-64

Download Full-Text

Persian Verion

View:

1,020

Download:

Cites:

Information Journal Paper

Title

STRUCTURAL ANALYSIS OF DOWGONBADAN REGION, ZAGROS FOLD THRUST BELT, AN INSTANCE OF FRONTAL AND LATERAL RAMP

Author(s)

NARIMANI H. | YASSAGHI A. | HASSAN GOODARZI M.GH. | Issue Writer Certificate

Keywords

ZAGROS FOLD-THRUST BELTQ2

TRANSVERSE FAULT ZONEQ2

FRONTAL AND LATERAL RAMPSQ2

MOUNTAIN FRONT FAULTQ2

DOWGONBADAN AREAQ2

Abstract

Structures in fold-thrust belts such as Zagros which are developing mainly along the belt strike often terminate at the transverse structures. The Zagros MOUNTAIN FRONT FAULT has cut and displace at different parts by transverse structures. At DOWGONBADAN AREA this fault is intersected by the Kharg-Mish transverse structure. The Mish anticline has transported fault propagation geometry and located on hanging wall of the MOUNTAIN FRONT FAULT. The anticline plunges and rotates when it reaches to the Kharg-Mish transverse fault to the west. In the fault footwall, however, the Dil, Pahn, Sarab and Jafarabad anticlines have rounded geometry and low amplitude show characteristics of the Dezful Embayment zone folds. The Dil and Pahn anticlines with bifurcate geometry and outcrop of Asmari Formation develop parallel to the frontal ramp strike and show footwall anticlines that propagated from the frontal ramp at Dashtak formation as delay structures with respect to the hanging wall structures. The Kharg-Mish fault identify as a lateral ramp on the surface by termination of longitudinal structures and at the depth with thickness and facies changes of the Ilam Formation. The structural characteristics of the Dowghonbadan area in the ZAGROS FOLD-THRUST BELT are analyzed as the interaction of the MOUNTAIN FRONT FAULT and the Kharg-Mish transverse fault as the FRONTAL AND LATERAL RAMPS, respectively.

Cites

No record.

References

No record.

Cite

APA: Copy

NARIMANI, H., YASSAGHI, A., & HASSAN GOODARZI, M.GH.. (2012). STRUCTURAL ANALYSIS OF DOWGONBADAN REGION, ZAGROS FOLD THRUST BELT, AN INSTANCE OF FRONTAL AND LATERAL RAMP. GEOSCIENCES, 21(82), 53-64. SID. https://sid.ir/paper/32520/en

Vancouver: Copy

NARIMANI H., YASSAGHI A., HASSAN GOODARZI M.GH.. STRUCTURAL ANALYSIS OF DOWGONBADAN REGION, ZAGROS FOLD THRUST BELT, AN INSTANCE OF FRONTAL AND LATERAL RAMP. GEOSCIENCES[Internet]. 2012;21(82):53-64. Available from: https://sid.ir/paper/32520/en

IEEE: Copy

H. NARIMANI, A. YASSAGHI, and M.GH. HASSAN GOODARZI, “STRUCTURAL ANALYSIS OF DOWGONBADAN REGION, ZAGROS FOLD THRUST BELT, AN INSTANCE OF FRONTAL AND LATERAL RAMP,” GEOSCIENCES, vol. 21, no. 82, pp. 53–64, 2012, [Online]. Available: https://sid.ir/paper/32520/en

Related Journal Papers