FACIES AND DEPOSITIONAL ENVIRONMENT OF CARBONATE ROCKS OF THE LOWER PERMIAN IN OZBAK-KUH OF EAST CENTRAL 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.

TAHERI A.A.GH.; GORGIJ M.N.; JAFARIAN M.A.

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

Journal Paper

Paper Information

Journal: RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE" Year:2001 | Volume:15 | Issue:1-2 Page(s): 93-112

Download Full-Text

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

Persian Verion

View:

930

Download:

Cites:

Information Journal Paper

Title

FACIES AND DEPOSITIONAL ENVIRONMENT OF CARBONATE ROCKS OF THE LOWER PERMIAN IN OZBAK-KUH OF EAST CENTRAL IRAN

Author(s)

TAHERI A.A.GH. | GORGIJ M.N. | JAFARIAN M.A. | Issue Writer Certificate

Keywords

Not Registered.

Abstract

Sediments of the Permian in zaladu section (East Central zone of Iran) are dominantly of sandstone and shale in the lower part and carbonate rocks in the middle and upper parts. The thickness of the sediments increases from north to south. Study of petrography indicates that carbonate sediments of the Lower Permian can be divided into several groups of carbonate microfacies. Microscopic studies and field observations show that the carbonate mirofacies form in four sub-sedimentary environments, including: tidal flat, lagoon, bar and open marine. The absence of build-up, Slump and turbidite currents indicate that the carbonate platform of the Lower Permian is a homoclinal ramp. Clastic sediments (sandstone and shale) are also observed at the base of succession. Type of sandstones, sedimentary structures, lateral continuity of beds and a gradual replacement of carbonate facies (upward), probably show a coastal or transitional sedimentation. Increasing water depth in the Lower Permian caused a decline in clastic input and an establishment of carbonate deposition. The sedimentation ended by decreasing water depth and exposure of sediments. An Eros ional surface is also present.

Cites

No record.

References

محیط رسوبی و توالی های سنگ های پرمین در منطقه بی بی شهربانو ،جنوب شرق تهران

Cite

APA: Copy

TAHERI, A.A.GH., GORGIJ, M.N., & JAFARIAN, M.A.. (2001). FACIES AND DEPOSITIONAL ENVIRONMENT OF CARBONATE ROCKS OF THE LOWER PERMIAN IN OZBAK-KUH OF EAST CENTRAL IRAN. RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", 15(1-2), 93-112. SID. https://sid.ir/paper/55880/en

Vancouver: Copy

TAHERI A.A.GH., GORGIJ M.N., JAFARIAN M.A.. FACIES AND DEPOSITIONAL ENVIRONMENT OF CARBONATE ROCKS OF THE LOWER PERMIAN IN OZBAK-KUH OF EAST CENTRAL IRAN. RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE"[Internet]. 2001;15(1-2):93-112. Available from: https://sid.ir/paper/55880/en

IEEE: Copy

A.A.GH. TAHERI, M.N. GORGIJ, and M.A. JAFARIAN, “FACIES AND DEPOSITIONAL ENVIRONMENT OF CARBONATE ROCKS OF THE LOWER PERMIAN IN OZBAK-KUH OF EAST CENTRAL IRAN,” RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", vol. 15, no. 1-2, pp. 93–112, 2001, [Online]. Available: https://sid.ir/paper/55880/en

Related Journal Papers