MICROFACIES, DEPOSITIONAL MODEL AND SEQUENCE STRATIGRAPHY OF DARIYAN FORMATION IN NORTHERN HIGH ZAGROS FAULT

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.

YAVARI M.; YAZDI M.; ADABI M.H.; GHALAVANDI H.

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

Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2016 | Volume:25 | Issue:100 Page(s): 281-290

Download Full-Text

Persian Verion

View:

1,024

Download:

Cites:

Information Journal Paper

Title

MICROFACIES, DEPOSITIONAL MODEL AND SEQUENCE STRATIGRAPHY OF DARIYAN FORMATION IN NORTHERN HIGH ZAGROS FAULT

Author(s)

YAVARI M. | YAZDI M. | ADABI M.H. | GHALAVANDI H. | Issue Writer Certificate

Keywords

DARIYAN FORMATIONQ2

MICROFACIESQ2

ZAGROSQ2

SEQUENCE STRATIGRAPHYQ2

KUH-E GADVANQ1

KUH-E BANESHQ1

Abstract

DARIYAN FORMATION deposited in two different sedimentary settings. In some places it consists of shallow Limestone with algae and Orbitolina and in the other places in addition to limestone, it represents black shales and marls associated with planktonic foraminifera and radiolarian. In this research Draiyan Formation was studied in order to MICROFACIES, depositional model and sequences stratigraphy of two sections so called, KUH-E GADVAN and KUH-E BANESH in high ZAGROS belt. Detailed petrographic studies led to the recognition of five main facies belts including: lagoon, bar, shallow open marine, outer ramp and deep marine. According to the vertical and lateral variations of facies, the DARIYAN FORMATION deposited on a carbonate ramp platform and intrashelf basin. Depositional sequences have been presented on the basis of analysis of facies, fauna assemblages, Gama and Neutron logs. Three 3 rd orders depositional sequences have been recognized during deposition of sediments. There is Type I sequence boundary in the top of third sequence and the other two sequences was considered as Type II sequence. Sea level fluctuations of the studied area correlated with Arabian platform and these changes follow of regional factors.

Cites

No record.

References

No record.

Cite

APA: Copy

YAVARI, M., YAZDI, M., ADABI, M.H., & GHALAVANDI, H.. (2016). MICROFACIES, DEPOSITIONAL MODEL AND SEQUENCE STRATIGRAPHY OF DARIYAN FORMATION IN NORTHERN HIGH ZAGROS FAULT. GEOSCIENCES, 25(100), 281-290. SID. https://sid.ir/paper/31695/en

Vancouver: Copy

YAVARI M., YAZDI M., ADABI M.H., GHALAVANDI H.. MICROFACIES, DEPOSITIONAL MODEL AND SEQUENCE STRATIGRAPHY OF DARIYAN FORMATION IN NORTHERN HIGH ZAGROS FAULT. GEOSCIENCES[Internet]. 2016;25(100):281-290. Available from: https://sid.ir/paper/31695/en

IEEE: Copy

M. YAVARI, M. YAZDI, M.H. ADABI, and H. GHALAVANDI, “MICROFACIES, DEPOSITIONAL MODEL AND SEQUENCE STRATIGRAPHY OF DARIYAN FORMATION IN NORTHERN HIGH ZAGROS FAULT,” GEOSCIENCES, vol. 25, no. 100, pp. 281–290, 2016, [Online]. Available: https://sid.ir/paper/31695/en

Related Journal Papers