Clinopyroxene mineral chemistry of Peshtasar basalts, sedimentary basin of Moghan (NW 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.

AMRAEE A.; Zareisahamieh r.; MOAYYED M.; Ahmadikhalaji a.; Azemzadeh a.

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

Journal Paper

Paper Information

Journal: Iranian Journal of Geology Year:2019 | Volume:12 | Issue:48 Page(s): 25-37

Download Full-Text

Persian Verion

View:

741

Download:

Cites:

Information Journal Paper

Title

Clinopyroxene mineral chemistry of Peshtasar basalts, sedimentary basin of Moghan (NW Iran)

Author(s)

Keywords

Peshtasar basaltQ1

Crystalization temperatureQ2

Mineral chemistryQ2

Clinopyroxene.Q1

Abstract

With the east– west exposure trend, Peshtasar basalts are in the sedimentary basin of Moghan (Talesh structural zone), in the northwest of Iran. The Peshtasar complex lithologically includes basalt, andesitic basalt or basaltic andesite, megaporphyric andesite, leucite tephrite and volcanic breccia. The main constituent minerals are plagioclase, Clinopyroxene. and iddingsitized olivine in basalts and plagioclase megacryst, Clinopyroxene. and leucite in tephrite. The results of the microprobe analyses of Clinopyroxene.reveal the diopside composition. Clinopyroxene. of Peshtasar basalts have igneous nature originated from alkaline and continental magmatic serries. The results of termobarometry studies indicate the crystallization range from 800-1200 degrees centigrade and crystallization pressure less than 5 kb. There was no water in composition of the parent magma of these rocks. The titanium contents of Clinopyroxene. were low, indicating the presence of titano-magnetite (opaque minerals) in the rock. The ferric iron values in Clinopyroxene. represents a high oxygen fugacity of magma.

Cites

No record.

References

No record.

Cite

APA: Copy

AMRAEE, A., Zareisahamieh, r., MOAYYED, M., Ahmadikhalaji, a., & Azemzadeh, a.. (2019). Clinopyroxene mineral chemistry of Peshtasar basalts, sedimentary basin of Moghan (NW Iran). IRANIAN JOURNAL OF GEOLOGY, 12(48 ), 25-37. SID. https://sid.ir/paper/129271/en

Vancouver: Copy

AMRAEE A., Zareisahamieh r., MOAYYED M., Ahmadikhalaji a., Azemzadeh a.. Clinopyroxene mineral chemistry of Peshtasar basalts, sedimentary basin of Moghan (NW Iran). IRANIAN JOURNAL OF GEOLOGY[Internet]. 2019;12(48 ):25-37. Available from: https://sid.ir/paper/129271/en

IEEE: Copy

A. AMRAEE, r. Zareisahamieh, M. MOAYYED, a. Ahmadikhalaji, and a. Azemzadeh, “Clinopyroxene mineral chemistry of Peshtasar basalts, sedimentary basin of Moghan (NW Iran),” IRANIAN JOURNAL OF GEOLOGY, vol. 12, no. 48 , pp. 25–37, 2019, [Online]. Available: https://sid.ir/paper/129271/en

Related Journal Papers