TECTONIC EVOLUTION AND STRUCTURAL MODEL OF AGHDARBAND TECTONIC WINDOW

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.

SHAHRIARI S.; GHAEMI F.; MOUSAVI HARAMI SEYED REZA; SAEEDI A.

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

Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2005 | Volume:14 | Issue:54 Page(s): 80-95

Download Full-Text

Persian Verion

View:

1,485

Download:

Cites:

Information Journal Paper

Title

TECTONIC EVOLUTION AND STRUCTURAL MODEL OF AGHDARBAND TECTONIC WINDOW

Author(s)

SHAHRIARI S. | GHAEMI F. | MOUSAVI HARAMI SEYED REZA | SAEEDI A. | Issue Writer Certificate

Keywords

AGHDARBAND TECTONIC WINDOWQ4

KOPET-DAGH BASINQ2

TURAN BLOCKQ4

PALEOTETHYSQ2

HERCYNIAN-CIMMERIAN AND ALPINE OROGENYQ4

THRUST FAULTQ4

Abstract

The basement of KOPET-DAGH BASIN is formed of pre-Jurassic rock units. The exposed units in Aghdarband area were strongly deformed during Hercynian, Cimmerian and Alpian orogenies. Hercynian orogeny generated metamorphism of green schist facies with strong faulting, whereas Cimmerian orogeny caused Triassic THRUST FAULTing. Alpine orogeny (Paleogene to Recent) causesd the folding of sediments of the KOPET-DAGH BASIN and had formed initially THRUST FAULTs and then, oblique slip faults (strike slip with reverse movement) in the region. These faults are still active.Rock units in the basement contain sedimentary and igneous rocks. The sedimentary rocks are composed mainly of volcanogenic siliciclastic sediments, including conglomerate, sandstone and shale (Devonian to Triassic age).The small outcrops of igneous rocks are exposed in the southwest of the Aghdarband area and include two rock units: 1-Darreh Anjir ophiolith complex that contains gabbro and ultramafic rocks.2- Acid tuffsThese rocks were mixed with ophiolithic rocks by THRUST FAULTs and appeared in the form of thin nappes.

Cites

No record.

References

یافته های جدید از سنگهای افیولیتی و سنگهای پالئوزوئیک پایانی در شمال خاوری خراسان (از جمله کپه داغ) و اهمیت ژئودینامیکی آنها

Cite

APA: Copy

SHAHRIARI, S., GHAEMI, F., MOUSAVI HARAMI, SEYED REZA, & SAEEDI, A.. (2005). TECTONIC EVOLUTION AND STRUCTURAL MODEL OF AGHDARBAND TECTONIC WINDOW. GEOSCIENCES, 14(54), 80-95. SID. https://sid.ir/paper/31677/en

Vancouver: Copy

SHAHRIARI S., GHAEMI F., MOUSAVI HARAMI SEYED REZA, SAEEDI A.. TECTONIC EVOLUTION AND STRUCTURAL MODEL OF AGHDARBAND TECTONIC WINDOW. GEOSCIENCES[Internet]. 2005;14(54):80-95. Available from: https://sid.ir/paper/31677/en

IEEE: Copy

S. SHAHRIARI, F. GHAEMI, SEYED REZA MOUSAVI HARAMI, and A. SAEEDI, “TECTONIC EVOLUTION AND STRUCTURAL MODEL OF AGHDARBAND TECTONIC WINDOW,” GEOSCIENCES, vol. 14, no. 54, pp. 80–95, 2005, [Online]. Available: https://sid.ir/paper/31677/en

Related Journal Papers