SEDIMENTARY ENVIRONMENT AND SEQUENCE STRATIGRAPHY OF FAHLIYAN FORMATION IN CENTER OF FARS

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.

RASTEGAR LARI A.R.

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

Journal Paper

Paper Information

Journal: JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY) Year:2009 | Volume:5 | Issue:2 Page(s): 111-120

Download Full-Text

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

Persian Verion

View:

844

Download:

Cites:

Information Journal Paper

Title

SEDIMENTARY ENVIRONMENT AND SEQUENCE STRATIGRAPHY OF FAHLIYAN FORMATION IN CENTER OF FARS

Author(s)

RASTEGAR LARI A.R. | Issue Writer Certificate

Keywords

KHAMI GROUPQ2

ARSENJANQ3

SIVANDQ3

TITHONIANQ3

VALLANGINIANQ3

Abstract

Fahliyan Formation (Volgian - Neocomian) (Early Cretaceous) is a part of KHAMI GROUP. This formation has been studied in two sections in center of Fars (southwest of ARSENJAN city and west of SIVAND city) to determine its facies, sedimentary environments and sequence Stratigraphy. The deposits of Fahlyian Formation consist of carbonate facies which are deposited in a Carbonate Rimmed Shelf. Two sequences with both type 1 and type 2 sequence boundaries are recognized within these deposits which are in accordance with a part of Zuni mega sequence (Lower Zuni III). The age of this formation is referred toTithonian- VALLANGINIAN (Early Cretaceous).

Cites

No record.

References

Cite

APA: Copy

RASTEGAR LARI, A.R.. (2009). SEDIMENTARY ENVIRONMENT AND SEQUENCE STRATIGRAPHY OF FAHLIYAN FORMATION IN CENTER OF FARS. JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY), 5(2), 111-120. SID. https://sid.ir/paper/127165/en

Vancouver: Copy

RASTEGAR LARI A.R.. SEDIMENTARY ENVIRONMENT AND SEQUENCE STRATIGRAPHY OF FAHLIYAN FORMATION IN CENTER OF FARS. JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY)[Internet]. 2009;5(2):111-120. Available from: https://sid.ir/paper/127165/en

IEEE: Copy

A.R. RASTEGAR LARI, “SEDIMENTARY ENVIRONMENT AND SEQUENCE STRATIGRAPHY OF FAHLIYAN FORMATION IN CENTER OF FARS,” JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY), vol. 5, no. 2, pp. 111–120, 2009, [Online]. Available: https://sid.ir/paper/127165/en

Related Journal Papers