SEQUENCE STRATIGRAPHY OF CARBONATE–EVAPORITE SUCCESSIONS OF DASHTAK FORMATION IN AGHAR#1AND WEST AGHAR#1 BOREHOLES IN AGHAR GAS FIELD

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.

KHOSHNOODKIA M.; MOHSENI H.; HAJIAN M.

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

Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2011 | Volume:20 | Issue:79 Page(s): 171-182

Download Full-Text

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

Persian Verion

View:

1,274

Download:

Cites:

Information Journal Paper

Title

SEQUENCE STRATIGRAPHY OF CARBONATE–EVAPORITE SUCCESSIONS OF DASHTAK FORMATION IN AGHAR#1AND WEST AGHAR#1 BOREHOLES IN AGHAR GAS FIELD

Author(s)

KHOSHNOODKIA M. | MOHSENI H. | HAJIAN M. | Issue Writer Certificate

Keywords

DASHTAK FORMATIONQ2

SEQUENCE STRATIGRAPHYQ2

RAMPQ2

AGHAR GAS FIELDQ2

COSTAL FARSQ2

Abstract

intervals of DASHTAK FORMATION is an important cap rocks in Zagros basin. Sequence stratigraphic analysis of Dashtak Carbonate–evaporates Formation in two wells (Aghar#1; West Aghar#1) was investigated in sequence stratigraphic framework. Data obtained from petrographic examinations of thin sections prepared from cuttings, in addition, a full suite of gamma ray and sonic logs were interpreted. DASHTAK FORMATION comprises eight facies belts that are: (i) detrital clastics, (ii) supratidal, (iii) tidal flat, (iv) lagoon, (v) shoal, (vi) restricted marine, (vii) open marine, (viii) mid RAMP. DASHTAK FORMATION consists of four sequences with four transgressive, regressive and maximum flooding surfaces. Two sequence boundaries type I and three sequence boundaries type II were recognized in the DASHTAK FORMATION. As far the depositional environment of the formation is interpreted as a homocline RAMP with mild lateral changes in depositional environment, hence negligible lateral changes of stratigraphic sequences are expected in the study area.

Cites

No record.

References

No record.

Cite

APA: Copy

KHOSHNOODKIA, M., MOHSENI, H., & HAJIAN, M.. (2011). SEQUENCE STRATIGRAPHY OF CARBONATE–EVAPORITE SUCCESSIONS OF DASHTAK FORMATION IN AGHAR#1AND WEST AGHAR#1 BOREHOLES IN AGHAR GAS FIELD. GEOSCIENCES, 20(79), 171-182. SID. https://sid.ir/paper/31552/en

Vancouver: Copy

KHOSHNOODKIA M., MOHSENI H., HAJIAN M.. SEQUENCE STRATIGRAPHY OF CARBONATE–EVAPORITE SUCCESSIONS OF DASHTAK FORMATION IN AGHAR#1AND WEST AGHAR#1 BOREHOLES IN AGHAR GAS FIELD. GEOSCIENCES[Internet]. 2011;20(79):171-182. Available from: https://sid.ir/paper/31552/en

IEEE: Copy

M. KHOSHNOODKIA, H. MOHSENI, and M. HAJIAN, “SEQUENCE STRATIGRAPHY OF CARBONATE–EVAPORITE SUCCESSIONS OF DASHTAK FORMATION IN AGHAR#1AND WEST AGHAR#1 BOREHOLES IN AGHAR GAS FIELD,” GEOSCIENCES, vol. 20, no. 79, pp. 171–182, 2011, [Online]. Available: https://sid.ir/paper/31552/en

Related Journal Papers