Petrographic and chemical investigation of the main minerals of gabbroic rocks in Javazm - Shahr Babak area located in Kerman Province, Iran

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.

Akmali Sheida; Moradian Abbas; Ahmadipour Hamid; Tiepolo Massimo

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:2025 | Volume:33 | Issue:1 Page(s): 135-152

Download Full-Text

Persian Verion

View:

Download:

Cites:

Information Journal Paper

Title

Petrographic and chemical investigation of the main minerals of gabbroic rocks in Javazm - Shahr Babak area located in Kerman Province, Iran

Author(s)

Akmali Sheida | Moradian Abbas | Ahmadipour Hamid | Tiepolo Massimo | Issue Writer Certificate

Keywords

Gabbro

gabbro pegmatite

chemistry of minerals

Javazm

Shahr-Babak

Kerman

Abstract

The studied area is located about 45 km northwest of Shahr-Babak, southeast of the Urumieh-Dokhtar volcanic belt, and is a part of the central Iran. In the Gabbro intrusive mass of this area, Gabbro pegmatite is observed, which indicates their deep origin. In plagioclase and pyroxenes, disequilibrium textures such as enclaves, sieve textures, and zoning are observed. Plagioclases are type andesine to bitonite. Pyroxenes are clinopyroxene (diopside) in the igneous range (subalkaline-tholeiitic). Also, these minerals are formed during orogeny in the volcanic arc setting. The formation temperature of plagioclase minerals ranges between 550 to 850 degrees Celsius and the temperature of clinopyroxene minerals is between 1180 to 1220 degrees Celsius. The pressure during the crystallization of clinopyroxene minerals ranges between 6 to 10 kbar. Environmentaly, the pyroxene minerals formed in the oxygen fugacity is high and the amount of magma water during magma crystallization is calculated to be about 10%. Olivines are hyalosiderite type and rich in magnesium.

Multimedia

No record.

Cites

No record.

References

No record.

Cite

Related Journal Papers

No record.

Related Seminar Papers

No record.

Related Plans