TECTONO-SEDIMENTARY SETTING OF SABZPUSHAN FAULT ZONE IN ZAGROS BASIN EVOLUTION, IRAN

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.

SAFARI H.

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

Journal Paper

Paper Information

Journal: SHAHID CHAMRAN UNIVERSITY JOURNAL OF SCIENCE Year:2006 | Volume:NEW SERIES | Issue:14 Page(s): 77-89

Download Full-Text

Persian Verion

View:

1,084

Download:

Cites:

Information Journal Paper

Title

TECTONO-SEDIMENTARY SETTING OF SABZPUSHAN FAULT ZONE IN ZAGROS BASIN EVOLUTION, IRAN

Author(s)

SAFARI H. | Issue Writer Certificate

Keywords

TECTONO-SEDIMENTARYQ4

FOLD-THRUST BELTQ3

FACIESQ4

TEAR FAULTQ3

SABZ PUSHAN FAULTQ4

EN ECHELON FOLDSQ4

ISOLITH MAPQ4

ISO FACIES MAPQ4

FACIES CHANGEQ4

Abstract

Zagros is a Fold thrust belt which is extended from North West to South Center of Iran. This mountain range is truncated and disturbed by TEAR FAULTs (with NWN-SES trend). Due to study of setting of these faults in evolution of Zagros basin, the SABZ PUSHAN FAULT zone is selected as a case study. FACIES and thickness contour maps controls and field investigations revealed that the fault zone was frequently active from Middle Cretaceous (Cenomanian) to recent time. From WSW to ENE, the main pieces of evidence of these activities are: A) thickness increase of Sarvak Fm, B) FACIES change of Gurpi shale and marl to Tarbur limestone, C) FACIES change of Pabdeh marl to limestone-dolomitic FACIES of lahrum Fm, D) FACIES change of Gachsaran evaporates and marls to multi-colored marls of Razak Fm, E) FACIES boundary of Mishan Fm and F) thickness increase of Aghajari Fm. and prevention of transportation of Bakhtiari Cherty component to WSW. Despite older activities of same TEAR FAULT in Zagros, no evidence of pre-middle Cretaceous activities of Sabz Pushan is documented.

Cites

No record.

References

تحلیل دگر ریختی های پهنه گسله عرضی برشی سبزپوشان

Cite

APA: Copy

SAFARI, H.. (2006). TECTONO-SEDIMENTARY SETTING OF SABZPUSHAN FAULT ZONE IN ZAGROS BASIN EVOLUTION, IRAN. SHAHID CHAMRAN UNIVERSITY JOURNAL OF SCIENCE, NEW SERIES(14), 77-89. SID. https://sid.ir/paper/58038/en

Vancouver: Copy

SAFARI H.. TECTONO-SEDIMENTARY SETTING OF SABZPUSHAN FAULT ZONE IN ZAGROS BASIN EVOLUTION, IRAN. SHAHID CHAMRAN UNIVERSITY JOURNAL OF SCIENCE[Internet]. 2006;NEW SERIES(14):77-89. Available from: https://sid.ir/paper/58038/en

IEEE: Copy

H. SAFARI, “TECTONO-SEDIMENTARY SETTING OF SABZPUSHAN FAULT ZONE IN ZAGROS BASIN EVOLUTION, IRAN,” SHAHID CHAMRAN UNIVERSITY JOURNAL OF SCIENCE, vol. NEW SERIES, no. 14, pp. 77–89, 2006, [Online]. Available: https://sid.ir/paper/58038/en

Related Journal Papers