TECTONOSTRATIGRAPHIC UNITS OF SOUTHEASTERN PART OF THE SANANDAJ-SIRJAN 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.

SHEIKHOLESLAMI M.R.

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

Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2015 | Volume:24 | Issue:95 (TECTONIC) Page(s): 243-252

Download Full-Text

Persian Verion

View:

1,468

Download:

Cites:

Information Journal Paper

Title

TECTONOSTRATIGRAPHIC UNITS OF SOUTHEASTERN PART OF THE SANANDAJ-SIRJAN ZONE

Author(s)

SHEIKHOLESLAMI M.R. | Issue Writer Certificate

Keywords

METAMORPHISMQ2

SANADAJ-SIRJAN ZONEQ2

TECTONOSTRATIGRAPHYQ2

NEOTETHYSQ2

ZAGROSQ2

Abstract

Different characteristics of the rock units and their stratigraphic relationships, as well as magmatic and metamorphic activities in the southern part of the Sanandaj-Sirjan Zone resulted in identification of different tectono-stratigraphic units based on their tectonic environments reflecting the opening and closure of the NEOTETHYS Ocean in southern Iran. The major tectono-stratigraphic units identified in this study are as follows: sediments deposited in the aulacogen setting in southern part of the Central Iranian platform of Paleozoic to Middle Triassic age; Triassic volcanic rocks and turbiditic sediments; low-grade flysch-type sediments of Jurassic-Early Cretaceous age deposited in a forearc basin; Lower Cretaceous carbonate platform sediments; suture zone-related rocks containing ophiolite, radilolarite and glaucophane schists; Tertiary flysch- type sediments containing exotic blocks of Lower Cretaceous carbonate, ophiolite and of the ZAGROS Formations formed over the edge of High ZAGROS zone; retro-arc foreland sediments of Central Iran which unconformably overlie the deformed rocks of northeastern part of the area; and finally post-orogenic molasse-type sediments resulted from post uplift erosion of the ZAGROS orogeny, deposited in the internal and marginal parts of the southern Sanandaj-Sirjan zone.

Cites

No record.

References

No record.

Cite

APA: Copy

SHEIKHOLESLAMI, M.R.. (2015). TECTONOSTRATIGRAPHIC UNITS OF SOUTHEASTERN PART OF THE SANANDAJ-SIRJAN ZONE. GEOSCIENCES, 24(95 (TECTONIC)), 243-252. SID. https://sid.ir/paper/31318/en

Vancouver: Copy

SHEIKHOLESLAMI M.R.. TECTONOSTRATIGRAPHIC UNITS OF SOUTHEASTERN PART OF THE SANANDAJ-SIRJAN ZONE. GEOSCIENCES[Internet]. 2015;24(95 (TECTONIC)):243-252. Available from: https://sid.ir/paper/31318/en

IEEE: Copy

M.R. SHEIKHOLESLAMI, “TECTONOSTRATIGRAPHIC UNITS OF SOUTHEASTERN PART OF THE SANANDAJ-SIRJAN ZONE,” GEOSCIENCES, vol. 24, no. 95 (TECTONIC), pp. 243–252, 2015, [Online]. Available: https://sid.ir/paper/31318/en

Related Journal Papers