Mineral chemistry, origin and magmatic evolution of Sarduiyeh batholith, southeast of Kerman

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.

Nazarinia a.; MORTAZAVI S.M.; ARVIN M.; POOSTI M.

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

Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2019 | Volume:29 | Issue:113 Page(s): 245-256

Download Full-Text

Persian Verion

View:

336

Download:

Cites:

Information Journal Paper

Title

Mineral chemistry, origin and magmatic evolution of Sarduiyeh batholith, southeast of Kerman

Author(s)

Nazarinia a. | MORTAZAVI S.M. | ARVIN M. | POOSTI M. | Issue Writer Certificate

Keywords

UrumiehQ2

Dokhtar magmatic zone Mineral Chemistry Batholith SarduiyehQ1

Abstract

The Oligocene Sarduiyeh batholith with NW-SE trend is located in the southeast of the Urumieh-Dokhtar magmatic zone in the Kerman province. This batholith intruded into the Eocene volcanic rocks that comprises of andesite, andesite basalt and subordinate basalt with pyroclastics rocks. The batholith consists of acidic-intermediate rocks such as diorite, tonalite, granodiorite and monzogranite. Mineral Chemistry of plagioclase crystals indicate that their composition varies between oligoclase and andesine with An 24-43 and calcic amphibole have magnesiohornblende compositions. Field, petrological and geochemical studies show that the Sarduiyeh batholith magma is I-type, metaluminous to weakly peraluminous and its belonging to calc-alkaline series. On the primitive mantle-normalized spider diagram, all samples are enriched in large ion lithophile elements such as U, K, Pb and Sr and depleted in high field strength elements such as Ti, Ta and Nb which are characteristics of the volcanic arc setting formed in an active continental margin. Based on geochemical studies, the Sarduiyeh batholith formed as a result of partial melting from metabasic rocks of lower crust.

Cites

No record.

References

No record.

Cite

APA: Copy

Nazarinia, a., MORTAZAVI, S.M., ARVIN, M., & POOSTI, M.. (2019). Mineral chemistry, origin and magmatic evolution of Sarduiyeh batholith, southeast of Kerman. GEOSCIENCES, 29(113 ), 245-256. SID. https://sid.ir/paper/31392/en

Vancouver: Copy

Nazarinia a., MORTAZAVI S.M., ARVIN M., POOSTI M.. Mineral chemistry, origin and magmatic evolution of Sarduiyeh batholith, southeast of Kerman. GEOSCIENCES[Internet]. 2019;29(113 ):245-256. Available from: https://sid.ir/paper/31392/en

IEEE: Copy

a. Nazarinia, S.M. MORTAZAVI, M. ARVIN, and M. POOSTI, “Mineral chemistry, origin and magmatic evolution of Sarduiyeh batholith, southeast of Kerman,” GEOSCIENCES, vol. 29, no. 113 , pp. 245–256, 2019, [Online]. Available: https://sid.ir/paper/31392/en

Related Journal Papers