DEPOSITION ENVIRONMENTS AND SEQUENCE STRATIGRAPHY OF THE KAZHDOMI AND SARVAK FORMATIONS IN THE NORTHWEST OF FARS PROVINCE, SOUTHWEST 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.

ASILIAN MAHABADI HOSSEIN; LASEMI Y.

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

Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2007 | Volume:16 | Issue:63 Page(s): 30-39

Download Full-Text

Persian Verion

View:

935

Download:

Cites:

Information Journal Paper

Title

DEPOSITION ENVIRONMENTS AND SEQUENCE STRATIGRAPHY OF THE KAZHDOMI AND SARVAK FORMATIONS IN THE NORTHWEST OF FARS PROVINCE, SOUTHWEST IRAN

Author(s)

ASILIAN MAHABADI HOSSEIN | LASEMI Y. | Issue Writer Certificate

Keywords

SEQUENCE STRATIGRAPHYQ2

DEPOSITIONAL ENVIRONMENTSQ3

KAZHDUMI AND SARVAK FORMATIONSQ3

NORTHWEST OF FARS PROVINCEQ3

SOUTHWEST IRANQ3

Abstract

The Kazhdomi and Sarvak Formations (Bangestan Group) are mainly composed of carbonate rocks. In order to study facies, DEPOSITIONAL ENVIRONMENTS and sequence stratigrphy of these formations in the NORTHWEST OF FARS PROVINCE, 4 stratigraphic sections including Namak Kangan, Khartang, Khormonj (Coastal Fars) and Shah neshin (Sub-coastal Fars) have been studied. Carbonate rocks of the Kazhdomi and Sarvak Formations have been deposited in tidal flat (A), lagoon (B), barrier (C) and open marine (D) facies belts. The sandstone facies of the Kazhdomi Formation (Sandstone tongues equivalent to Burgan Sandstone) are quartzarenite, which were probably deposited in a beach environment. Facies analysis and comparison with Modern and ancient environments indicate that the Kazhdomi and Sarvak Formations were deposited in a ramp platform.SEQUENCE STRATIGRAPHY of the Bangestan Group in the study area indicate that the Kazhdomi Formation (except for Namak Kangan,which consists of one depositional sequence) include two depositional sequences (sequences 1 and 2) of early to late Albian age. The Sarvak Formation consists of one depositional sequence in Namak Kangan (sequence 3) and four sequences I (sequences 3 to 6) of late Albian to Turonian age in other sections.The lower contact of sequence 1, t he lower contact of sequence 2 in Namak Kangan and the lower and upper contacts of sequence 6 are type 1 unconformity (SB 1) but the contact of other sequences are type 2 unconformity (SB2).

Cites

References

بررسی میکروفاسیسها و محیط رسوبی سازند سروک در مناطق خوزستان و لرستان

Cite

APA: Copy

ASILIAN MAHABADI, HOSSEIN, & LASEMI, Y.. (2007). DEPOSITION ENVIRONMENTS AND SEQUENCE STRATIGRAPHY OF THE KAZHDOMI AND SARVAK FORMATIONS IN THE NORTHWEST OF FARS PROVINCE, SOUTHWEST IRAN. GEOSCIENCES, 16(63), 30-39. SID. https://sid.ir/paper/31780/en

Vancouver: Copy

ASILIAN MAHABADI HOSSEIN, LASEMI Y.. DEPOSITION ENVIRONMENTS AND SEQUENCE STRATIGRAPHY OF THE KAZHDOMI AND SARVAK FORMATIONS IN THE NORTHWEST OF FARS PROVINCE, SOUTHWEST IRAN. GEOSCIENCES[Internet]. 2007;16(63):30-39. Available from: https://sid.ir/paper/31780/en

IEEE: Copy

HOSSEIN ASILIAN MAHABADI, and Y. LASEMI, “DEPOSITION ENVIRONMENTS AND SEQUENCE STRATIGRAPHY OF THE KAZHDOMI AND SARVAK FORMATIONS IN THE NORTHWEST OF FARS PROVINCE, SOUTHWEST IRAN,” GEOSCIENCES, vol. 16, no. 63, pp. 30–39, 2007, [Online]. Available: https://sid.ir/paper/31780/en

Related Journal Papers