BIOSTRATIGRAPHY, MICROFACIES AND DEPOSITIONAL ENVIRONMENT THE ASMARI FORMATION IN NORTH OF THE MOKHTAR ANTICLINE, NORTHWEST YASUJ

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.

RIKHTEHGARZADEH M.; SEYRAFIAN A.; SAFARI A.; VAZIRI-MOGHADDAM H.

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

Journal Paper

Paper Information

Journal: RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE" Year:2008 | Volume:34 | Issue:5 (GEOLOGY) Page(s): 55-78

Download Full-Text

Persian Verion

View:

948

Download:

Cites:

Information Journal Paper

Title

BIOSTRATIGRAPHY, MICROFACIES AND DEPOSITIONAL ENVIRONMENT THE ASMARI FORMATION IN NORTH OF THE MOKHTAR ANTICLINE, NORTHWEST YASUJ

Author(s)

RIKHTEHGARZADEH M. | SEYRAFIAN A. | SAFARI A. | VAZIRI-MOGHADDAM H. | Issue Writer Certificate

Keywords

ASMARI FORMATIONQ3

BIOSTRATIGRAPHYQ3

MICROFACIESQ3

OLIGOCENE-MIOCENEQ3

Abstract

The ASMARI FORMATION with a thickness of 294m located at the north of Mokhtar Anticline 5 km northwest Yasuj. This formation was studied from biostratigrarphy, MICROFACIES and sedimentary environment point of view. Study of benthic foraminifera led to recognition of 31 genera and 20 species.Based on the distribution of foraminifera, three assemblage zones were identified. The Late Oligocene (Chattian) - Early Miocene (Aquitanian-Burdigalian) is suggested for the ASMARI FORMATION at the study area. Based on laboratory studies, 9 MICROFACIES related to 3 subenvironments (lagoon, bar and open marine) were identified. This study revealed that, the ASMARI FORMATION deposited on an homoclinal epicontinental carbonate ramp.

Cites

BIOSTRATIGRAPHY AND CARBONATE SKELETAL COMPONENTS OF THE ASMARI AND RAZAK FORMATIONS IN SOUTHEASTERN OF YASUJ (TANG-E SURKH SECTION)

References

No record.

Cite

APA: Copy

RIKHTEHGARZADEH, M., SEYRAFIAN, A., SAFARI, A., & VAZIRI-MOGHADDAM, H.. (2008). BIOSTRATIGRAPHY, MICROFACIES AND DEPOSITIONAL ENVIRONMENT THE ASMARI FORMATION IN NORTH OF THE MOKHTAR ANTICLINE, NORTHWEST YASUJ. RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", 34(5 (GEOLOGY)), 55-78. SID. https://sid.ir/paper/55834/en

Vancouver: Copy

RIKHTEHGARZADEH M., SEYRAFIAN A., SAFARI A., VAZIRI-MOGHADDAM H.. BIOSTRATIGRAPHY, MICROFACIES AND DEPOSITIONAL ENVIRONMENT THE ASMARI FORMATION IN NORTH OF THE MOKHTAR ANTICLINE, NORTHWEST YASUJ. RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE"[Internet]. 2008;34(5 (GEOLOGY)):55-78. Available from: https://sid.ir/paper/55834/en

IEEE: Copy

M. RIKHTEHGARZADEH, A. SEYRAFIAN, A. SAFARI, and H. VAZIRI-MOGHADDAM, “BIOSTRATIGRAPHY, MICROFACIES AND DEPOSITIONAL ENVIRONMENT THE ASMARI FORMATION IN NORTH OF THE MOKHTAR ANTICLINE, NORTHWEST YASUJ,” RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", vol. 34, no. 5 (GEOLOGY), pp. 55–78, 2008, [Online]. Available: https://sid.ir/paper/55834/en

Related Journal Papers