DEPOSITIONAL ENVIRONMENT AND SEQUENCE STRATIGRAPHY OF THE PABDEH FORMATION IN SHIRAZ AREA

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.

MIRZAEE MAHMOODABADI R.; LASEMI Y.; AFGHAH M.

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

Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2009 | Volume:19 | Issue:73 Page(s): 139-146

Download Full-Text

Persian Verion

View:

1,487

Download:

Cites:

Information Journal Paper

Title

DEPOSITIONAL ENVIRONMENT AND SEQUENCE STRATIGRAPHY OF THE PABDEH FORMATION IN SHIRAZ AREA

Author(s)

MIRZAEE MAHMOODABADI R. | LASEMI Y. | AFGHAH M. | Issue Writer Certificate

Keywords

PABDEH FORMATIONQ2

SHIRAZQ3

PURPLE SHALEQ3

ZANJIRAN SECTIONQ3

SHAHNESHIN SECTIONQ3

DEPOSITIONAL SEQUENCEQ3

Abstract

Shaley PABDEH FORMATION (Paleocene-Oligomiocene) expanded in Fars, Khozestan and Lorestan. Lower Lithostratigraphical limit with Gurpi Formation recognized by PURPLE SHALE. Upper Lithostratigraphical limith with Asmari Formation is transitional. In order to study sedimentary environments and sequence stratigraphy of PABDEH FORMATION two stratigraphic sections were chosen (Zanjiran and Shahneshin). Petrographic study indicated 9 pelagic and calciturbidite microfacies. These microfacies in deep marine deposited. Calciturbidite facies were formed during sea level highstand, when high rate of carbonate production result in transportation of carbonate sediment in deep sea. Sequence stratigraphy study shows that PABDEH FORMATION consists of two DEPOSITIONAL SEQUENCEs. In ZANJIRAN SECTION lower and upper contact of first sequence is type two and upper contact of second DEPOSITIONAL SEQUENCE is conformity with unconformity. In SHAHNESHIN SECTION the lower contact is type two and upper contact is correlative conformity with unconformity.

Cites

No record.

References

چینه نگاری سازند سروک در جنوب خاور لرستان و شمال زون ایذه و کاربرد آن در اکتشاف هیدروکربور

Cite

APA: Copy

MIRZAEE MAHMOODABADI, R., LASEMI, Y., & AFGHAH, M.. (2009). DEPOSITIONAL ENVIRONMENT AND SEQUENCE STRATIGRAPHY OF THE PABDEH FORMATION IN SHIRAZ AREA. GEOSCIENCES, 19(73), 139-146. SID. https://sid.ir/paper/32575/en

Vancouver: Copy

MIRZAEE MAHMOODABADI R., LASEMI Y., AFGHAH M.. DEPOSITIONAL ENVIRONMENT AND SEQUENCE STRATIGRAPHY OF THE PABDEH FORMATION IN SHIRAZ AREA. GEOSCIENCES[Internet]. 2009;19(73):139-146. Available from: https://sid.ir/paper/32575/en

IEEE: Copy

R. MIRZAEE MAHMOODABADI, Y. LASEMI, and M. AFGHAH, “DEPOSITIONAL ENVIRONMENT AND SEQUENCE STRATIGRAPHY OF THE PABDEH FORMATION IN SHIRAZ AREA,” GEOSCIENCES, vol. 19, no. 73, pp. 139–146, 2009, [Online]. Available: https://sid.ir/paper/32575/en

Related Journal Papers