MINERAL CHEMISTRY OF CLINOPYROXENES IN THE IGNEOUS ROCKS OF AMLASH AREA, NORTH 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.

KANANIAN A.; SALAVATI M.; ESMAEILI DARYOUSH; ASIABANHA A.

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

Journal Paper

Paper Information

Journal: JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT) Year:2005 | Volume:30 | Issue:2 Page(s): 229-245

Download Full-Text

Persian Verion

View:

1,451

Download:

Cites:

Information Journal Paper

Title

MINERAL CHEMISTRY OF CLINOPYROXENES IN THE IGNEOUS ROCKS OF AMLASH AREA, NORTH IRAN

Author(s)

KANANIAN A. | SALAVATI M. | ESMAEILI DARYOUSH | ASIABANHA A. | Issue Writer Certificate

Keywords

CLINOPYROXENEQ4

AMLASHQ4

BASALTQ3

GABBROQ3

GEOTHERMOMETRYQ4

Abstract

Igneous rocks, a part of a dismembered ophiolitic complex, cropping out in the south of AMLASH, are mostly composed of BASALTic lavas, doleritic dikes, GABBROic and pyroxenitic intrusions. CLINOPYROXENEs in these rocks are generally augite and diopside, which belong to calcic pyroxene category. Distribution of Si and Al in CLINOPYROXENE composition demonstrates these minerals are high Al pyroxenes. All si cations with some Al cations enter into tetrahedral sites and the rest of Al occupies the octahedral sites. The distributions of Al at tetra-and octahedral sites may suggest that the CLINOPYROXENEs crystallized at low pressure in a water bearing magma. The content of Fe+ 3 in the pyroxene composition is the direct result of higher 02 fugacity in magma chamber. The temperature of magma crystallization is evaluated from CLINOPYROXENE composition between 900-1100°C.

Multimedia

No record.

Cites

References

تفکیک بخش های مختلف ایران از نظر وضع ساختمانی در ارتباط با حوضه های رسوبی

Cite

APA: Copy

KANANIAN, A., SALAVATI, M., ESMAEILI, DARYOUSH, & ASIABANHA, A.. (2005). MINERAL CHEMISTRY OF CLINOPYROXENES IN THE IGNEOUS ROCKS OF AMLASH AREA, NORTH IRAN. JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT), 30(2), 229-245. SID. https://sid.ir/paper/2236/en

Vancouver: Copy

KANANIAN A., SALAVATI M., ESMAEILI DARYOUSH, ASIABANHA A.. MINERAL CHEMISTRY OF CLINOPYROXENES IN THE IGNEOUS ROCKS OF AMLASH AREA, NORTH IRAN. JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT)[Internet]. 2005;30(2):229-245. Available from: https://sid.ir/paper/2236/en

IEEE: Copy

A. KANANIAN, M. SALAVATI, DARYOUSH ESMAEILI, and A. ASIABANHA, “MINERAL CHEMISTRY OF CLINOPYROXENES IN THE IGNEOUS ROCKS OF AMLASH AREA, NORTH IRAN,” JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT), vol. 30, no. 2, pp. 229–245, 2005, [Online]. Available: https://sid.ir/paper/2236/en

Related Journal Papers