MICROFACIES, SEDIMENTARY ENVIRONMENT, SEQUENCE STRATIGRAPHY AND STRONTIUM DATING OF THE DASHTAK FORMATION IN THE PERSIAN GULF, FARS AND IZEH REGIONS

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.

HAJIAN BARZI M.; ALEALI M.; JAHANI D.; FALAH KHEYRKHAH M.

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

Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2015 | Volume:24 | Issue:95 (STRATIGRAPHY & SEDIMENTOLOGY) Page(s): 185-198

Download Full-Text

Persian Verion

View:

940

Download:

Cites:

Information Journal Paper

Title

MICROFACIES, SEDIMENTARY ENVIRONMENT, SEQUENCE STRATIGRAPHY AND STRONTIUM DATING OF THE DASHTAK FORMATION IN THE PERSIAN GULF, FARS AND IZEH REGIONS

Author(s)

HAJIAN BARZI M. | ALEALI M. | JAHANI D. | FALAH KHEYRKHAH M. | Issue Writer Certificate

Keywords

DASHTAK FORMATIONQ2

MICROFACIESQ2

CARBONATE RAMPQ3

SEQUENCE STRATIGRAPHYQ2

STRONTIUM ISOTOPEQ2

Abstract

The Middle- Late Triassic DASHTAK FORMATION acts as one of the best seal for giant gas reservoirs entrapped within the Dehram group inthe Southwest of Iran and the northern Persian Gulf because ofthick anhydrite deposits. The facies analysis of DASHTAK FORMATION led to recognition of 14 MICROFACIES, which are related to coastal plain, sabkha) supratidal (, tidal flat, lagoon, and shoal environments. Examination of the vertical and lateral facies changes and thire comparison with their modern and ancient counterparts, all indicate that the DASHTAK FORMATION was deposited in a shallow CARBONATE RAMP platform. The sequence stratigraphic studies showed that the DASHTAK FORMATION consists of four thirdorder depositional sequences, each consisting of the transgressive and highstand systems tracts. The thickness of this formation increases from the Kuh-e Surmeh toward the boreholes d, c, b and a. A STRONTIUM ISOTOPE dating of the DASHTAK FORMATION indicated a Triassic age from Ansian to Norian stages.

Cites

No record.

References

No record.

Cite

APA: Copy

HAJIAN BARZI, M., ALEALI, M., JAHANI, D., & FALAH KHEYRKHAH, M.. (2015). MICROFACIES, SEDIMENTARY ENVIRONMENT, SEQUENCE STRATIGRAPHY AND STRONTIUM DATING OF THE DASHTAK FORMATION IN THE PERSIAN GULF, FARS AND IZEH REGIONS. GEOSCIENCES, 24(95 (STRATIGRAPHY & SEDIMENTOLOGY)), 185-198. SID. https://sid.ir/paper/31599/en

Vancouver: Copy

HAJIAN BARZI M., ALEALI M., JAHANI D., FALAH KHEYRKHAH M.. MICROFACIES, SEDIMENTARY ENVIRONMENT, SEQUENCE STRATIGRAPHY AND STRONTIUM DATING OF THE DASHTAK FORMATION IN THE PERSIAN GULF, FARS AND IZEH REGIONS. GEOSCIENCES[Internet]. 2015;24(95 (STRATIGRAPHY & SEDIMENTOLOGY)):185-198. Available from: https://sid.ir/paper/31599/en

IEEE: Copy

M. HAJIAN BARZI, M. ALEALI, D. JAHANI, and M. FALAH KHEYRKHAH, “MICROFACIES, SEDIMENTARY ENVIRONMENT, SEQUENCE STRATIGRAPHY AND STRONTIUM DATING OF THE DASHTAK FORMATION IN THE PERSIAN GULF, FARS AND IZEH REGIONS,” GEOSCIENCES, vol. 24, no. 95 (STRATIGRAPHY & SEDIMENTOLOGY), pp. 185–198, 2015, [Online]. Available: https://sid.ir/paper/31599/en

Related Journal Papers