MINERALOGY AND PETROLOGY IN MAGMATIC ROCKS OF HORMOZ FORMATION (SALT DIAPIRES OF HIGH ZAGROS)

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.

TAGHIPOUR S.; KHALILI MAHMOUD; NOGHREHEIAN M.; TORABI GH.; MAKIZADEH M.A.; TAGHIPOUR B.

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

Journal Paper

Paper Information

Journal: IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY Year:2008 | Volume:16 | Issue:3 Page(s): 377-388

Download Full-Text

Persian Verion

View:

1,940

Download:

Cites:

Information Journal Paper

Title

MINERALOGY AND PETROLOGY IN MAGMATIC ROCKS OF HORMOZ FORMATION (SALT DIAPIRES OF HIGH ZAGROS)

Author(s)

Keywords

IRANQ2

HIGH ZAGROSQ2

SALT DOMEQ2

IGNEOUS ROCKSQ3

CLINOPYROXENEQ2

TRANSITIONAL MAGMAQ3

Abstract

Several igneous-evaporitic rocks complexes, belonging to Lower Cambrian, are exposed in High Zagros. These rocks exposed parallel to the Zagros main thrust as diapir-shaped bodies. Basaltic rocks are the most common rocks but microgabbro, microdiorite, andesite and trachyte are the rocks of this complex. The studied clinopyroxenes are usually fresh mafic mineral in these rocks and display sector zoning features. On the base of mineralogy and mineral chemistry, the pyroxenes are in the range of titan-augite to diopside composition. The geochemical study of the clinopyroxene as well as the discrimination diagrams were used in this study, point to the transitional to alkaline nature of magmatism which occurredv in a within continental plate rift environment.

Multimedia

No record.

Cites

References

جایگاه گنبدهای نمکی منطقه زاگرس بلند در ستون چینه سازی ایران

Cite

APA: Copy

TAGHIPOUR, S., KHALILI, MAHMOUD, NOGHREHEIAN, M., TORABI, GH., MAKIZADEH, M.A., & TAGHIPOUR, B.. (2008). MINERALOGY AND PETROLOGY IN MAGMATIC ROCKS OF HORMOZ FORMATION (SALT DIAPIRES OF HIGH ZAGROS). IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 16(3), 377-388. SID. https://sid.ir/paper/4039/en

Vancouver: Copy

TAGHIPOUR S., KHALILI MAHMOUD, NOGHREHEIAN M., TORABI GH., MAKIZADEH M.A., TAGHIPOUR B.. MINERALOGY AND PETROLOGY IN MAGMATIC ROCKS OF HORMOZ FORMATION (SALT DIAPIRES OF HIGH ZAGROS). IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2008;16(3):377-388. Available from: https://sid.ir/paper/4039/en

IEEE: Copy

S. TAGHIPOUR, MAHMOUD KHALILI, M. NOGHREHEIAN, GH. TORABI, M.A. MAKIZADEH, and B. TAGHIPOUR, “MINERALOGY AND PETROLOGY IN MAGMATIC ROCKS OF HORMOZ FORMATION (SALT DIAPIRES OF HIGH ZAGROS),” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 16, no. 3, pp. 377–388, 2008, [Online]. Available: https://sid.ir/paper/4039/en

Related Journal Papers