THE RELATION BETWEEN GLAUCONITIZATION AND CALCITE CEMENTATION WITH THE RELATIVE SEA LEVEL CHANGES IN THE MIXED SILISICLASTIC- CARBONATE SEDIMENTS OF AITAMIR FORMATION (MID-CRETACEOUS), KOPET-DAGH BASIN

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.

SHARAFI M.; MAHBOUBI A.; MOUSSAVI HARAMI R.

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

Journal Paper

Paper Information

Journal: JOURNAL OF STRATIGRAPHY AND SEDIMENTOLOGY RESEARCHES Year:2012 | Volume:28 | Issue:3 (48) Page(s): 19-36

Download Full-Text

Persian Verion

View:

1,171

Download:

Cites:

Information Journal Paper

Title

THE RELATION BETWEEN GLAUCONITIZATION AND CALCITE CEMENTATION WITH THE RELATIVE SEA LEVEL CHANGES IN THE MIXED SILISICLASTIC- CARBONATE SEDIMENTS OF AITAMIR FORMATION (MID-CRETACEOUS), KOPET-DAGH BASIN

Author(s)

SHARAFI M. | MAHBOUBI A. | MOUSSAVI HARAMI R. | Issue Writer Certificate

Keywords

AITAMIR FORMATIONQ2

DIAGENESISQ2

GLAUCONITIZATIONQ2

SEA LEVELQ2

TRANSGRESSIVE FACIESQ2

REGRESSIVE FACIESQ2

Abstract

Two diagenetic processes of GLAUCONITIZATION and calcite cementation and relation those to SEA LEVEL changes in the siliciclastic-carbonate sediments of the AITAMIR FORMATION (Albian-Cenomanian) in Kopet-Dagh basin have studied. The lower sandstone unit consists of mainly sandstone intercalated with shale and limestone and the upper shale units are two major sediments of this formation. The sandstone of the lower unit based on composition and their relations with SEA LEVEL change subdivided into two transgressive and REGRESSIVE FACIES and in this relation, show different pathways of the DIAGENESIS. In the TRANSGRESSIVE FACIES display by high content of the shell remains, with development in DIAGENESIS shows extensive cementation and a little compaction during burial stage. In the regressive sandstone, characterized by little skeletal elements, display little calcite cements and high burial compaction. The glauconitic grains and calcite cementation in the AITAMIR FORMATION concentrated in the TRANSGRESSIVE FACIES and especially in the maximum flooding surface and transgresive surface. Whereas, in the REGRESSIVE FACIES the glauconitic grains and calcite cementation is principally low. Moreover, the transgressive system tract and maximum flooding surface is characterized by mature and high mature glauconitic grains.

Cites

No record.

References

Cite

APA: Copy

SHARAFI, M., MAHBOUBI, A., & MOUSSAVI HARAMI, R.. (2012). THE RELATION BETWEEN GLAUCONITIZATION AND CALCITE CEMENTATION WITH THE RELATIVE SEA LEVEL CHANGES IN THE MIXED SILISICLASTIC- CARBONATE SEDIMENTS OF AITAMIR FORMATION (MID-CRETACEOUS), KOPET-DAGH BASIN. JOURNAL OF STRATIGRAPHY AND SEDIMENTOLOGY RESEARCHES, 28(3 (48)), 19-36. SID. https://sid.ir/paper/157077/en

Vancouver: Copy

SHARAFI M., MAHBOUBI A., MOUSSAVI HARAMI R.. THE RELATION BETWEEN GLAUCONITIZATION AND CALCITE CEMENTATION WITH THE RELATIVE SEA LEVEL CHANGES IN THE MIXED SILISICLASTIC- CARBONATE SEDIMENTS OF AITAMIR FORMATION (MID-CRETACEOUS), KOPET-DAGH BASIN. JOURNAL OF STRATIGRAPHY AND SEDIMENTOLOGY RESEARCHES[Internet]. 2012;28(3 (48)):19-36. Available from: https://sid.ir/paper/157077/en

IEEE: Copy

M. SHARAFI, A. MAHBOUBI, and R. MOUSSAVI HARAMI, “THE RELATION BETWEEN GLAUCONITIZATION AND CALCITE CEMENTATION WITH THE RELATIVE SEA LEVEL CHANGES IN THE MIXED SILISICLASTIC- CARBONATE SEDIMENTS OF AITAMIR FORMATION (MID-CRETACEOUS), KOPET-DAGH BASIN,” JOURNAL OF STRATIGRAPHY AND SEDIMENTOLOGY RESEARCHES, vol. 28, no. 3 (48), pp. 19–36, 2012, [Online]. Available: https://sid.ir/paper/157077/en

Related Journal Papers