GEOCHEMISTRY OF AHVAZ SANDSTONE MEMBER OF ASMARI FORMATION IN AHVAZ OIL FIELD: APPLICATION FOR TECTONIC PROVENANCE AND SOURCE ROCK WEATHERING

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.

HOSSEINI BARZI M.; JAFARZADEH MAHDI; ADAABI M.H.

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

Journal Paper

Paper Information

Journal: SHAHID CHAMRAN UNIVERSITY JOURNAL OF SCIENCE Year:2008 | Volume:NEW SERIES | Issue:19 (SECTION B) Page(s): 34-45

Download Full-Text

Persian Verion

View:

1,686

Download:

Cites:

Information Journal Paper

Title

GEOCHEMISTRY OF AHVAZ SANDSTONE MEMBER OF ASMARI FORMATION IN AHVAZ OIL FIELD: APPLICATION FOR TECTONIC PROVENANCE AND SOURCE ROCK WEATHERING

Author(s)

HOSSEINI BARZI M. | JAFARZADEH MAHDI | ADAABI M.H. | Issue Writer Certificate

Keywords

AHVAZ SANDSTONEQ3

PROVENANCEQ3

GEOCHEMISTRYQ3

WEATHERINGQ3

CRATONQ3

Abstract

Geochemical analysis of 9 samples from two subsurface sections (well No. Az 85 & well No. Az 11) of AHVAZ SANDSTONE Member of Asmari Formation in Ahvaz oil field were plotted on sandstones classification diagrams. Based on these data, sandstones are quartzarenite, subarkose and sublitharenite. Also, geochemical studies using discrimination, biplot and ternary diagrams determined the quartzose recycled PROVENANCE (craton and recycled orogen) and passive margin tectonic setting for these sandstones. Also, determination of WEATHERING index of sandstones in source area, with the use of CIW’ index represented medium WEATHERING index for these sandstones in the source area. However, this subject can be explained by arid to semi-arid climate in the recycled orogen. These conclusions are in harmony with deposition of these' sandstone~ over passive margins of Asmari forland basin.

Cites

ژئوشیمی گلسنگ ها و ماسه سنگ های میوسن پسین-پلئیستوسن منطقه ساحلی چابهار: با نگرشی بر سنگ منشا و جایگاه زمین ساختی

References

LITHOFACIES, SEDIMENTARY ENVIRONMENT AND PROVENANCE OF MIXED SILICICLASTIC-CARBONATE-EVAPORATE DEPOSITIONS OF ASMARI FORMATION IN AHWAZ OIL FIELD WITH REFERENCE TO MIXING MECHANISMS

Cite

APA: Copy

HOSSEINI BARZI, M., JAFARZADEH, MAHDI, & ADAABI, M.H.. (2008). GEOCHEMISTRY OF AHVAZ SANDSTONE MEMBER OF ASMARI FORMATION IN AHVAZ OIL FIELD: APPLICATION FOR TECTONIC PROVENANCE AND SOURCE ROCK WEATHERING. SHAHID CHAMRAN UNIVERSITY JOURNAL OF SCIENCE, NEW SERIES(19 (SECTION B)), 34-45. SID. https://sid.ir/paper/58029/en

Vancouver: Copy

HOSSEINI BARZI M., JAFARZADEH MAHDI, ADAABI M.H.. GEOCHEMISTRY OF AHVAZ SANDSTONE MEMBER OF ASMARI FORMATION IN AHVAZ OIL FIELD: APPLICATION FOR TECTONIC PROVENANCE AND SOURCE ROCK WEATHERING. SHAHID CHAMRAN UNIVERSITY JOURNAL OF SCIENCE[Internet]. 2008;NEW SERIES(19 (SECTION B)):34-45. Available from: https://sid.ir/paper/58029/en

IEEE: Copy

M. HOSSEINI BARZI, MAHDI JAFARZADEH, and M.H. ADAABI, “GEOCHEMISTRY OF AHVAZ SANDSTONE MEMBER OF ASMARI FORMATION IN AHVAZ OIL FIELD: APPLICATION FOR TECTONIC PROVENANCE AND SOURCE ROCK WEATHERING,” SHAHID CHAMRAN UNIVERSITY JOURNAL OF SCIENCE, vol. NEW SERIES, no. 19 (SECTION B), pp. 34–45, 2008, [Online]. Available: https://sid.ir/paper/58029/en

Related Journal Papers