THE STUDY OF CHEMICAL COMPOSITION, ZONING AND GENESIS OF GARNET CRYSTALS IN THE METAMORPHIC AND IGNEOUS ROCKS IN THE HAMADAN AREA

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.

HOSSEIN MIRZAEE ZAHRA; DADKHAH R.; HOSSEIN MIRZAEE ZOHREH

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

Journal Paper

Paper Information

Journal: Iranian Journal of Geology Year:2011 | Volume:5 | Issue:19 Page(s): 3-14

Download Full-Text

Persian Verion

View:

1,744

Download:

Cites:

Information Journal Paper

Title

THE STUDY OF CHEMICAL COMPOSITION, ZONING AND GENESIS OF GARNET CRYSTALS IN THE METAMORPHIC AND IGNEOUS ROCKS IN THE HAMADAN AREA

Author(s)

HOSSEIN MIRZAEE ZAHRA | DADKHAH R. | HOSSEIN MIRZAEE ZOHREH | Issue Writer Certificate

Keywords

EVIDENT ZONINGQ2

HIDDEN ZONINGQ2

MIXED ZONINGQ2

GARNETQ2

HAMEDANQ2

Abstract

The study area is a part of the Sanandaj- Sirjan metamorphic belt. Hamadan metamorphic rocks can be divided into three groups: regional metamorphic rocks, contact metamorphic rocks and migmatites. GARNET crystals are usually common in all of the metamorphic rocks (except slate and phyllite) and in the igneous rocks (i.e. aplite, pegmatite and monzogranite). They fall in pyralspite group and are rich in almandine. Some of these GARNETs illustrate zoning which can be divided into three groups: EVIDENT ZONING, HIDDEN ZONING and MIXED ZONING. Origin of observed GARNET crystals is metamorphic and igneous. GARNET crystals in the regional metamorphic rocks, contact metamorphic rocks, mesosome and melanosome of migmatites and GARNET monzogranites have metamorphic origin. These crystals in the GARNET aplites and GARNET pegmatites have igneous origin.

Cites

No record.

References

No record.

Cite

APA: Copy

HOSSEIN MIRZAEE, ZAHRA, DADKHAH, R., & HOSSEIN MIRZAEE, ZOHREH. (2011). THE STUDY OF CHEMICAL COMPOSITION, ZONING AND GENESIS OF GARNET CRYSTALS IN THE METAMORPHIC AND IGNEOUS ROCKS IN THE HAMADAN AREA. IRANIAN JOURNAL OF GEOLOGY, 5(19), 3-14. SID. https://sid.ir/paper/129431/en

Vancouver: Copy

HOSSEIN MIRZAEE ZAHRA, DADKHAH R., HOSSEIN MIRZAEE ZOHREH. THE STUDY OF CHEMICAL COMPOSITION, ZONING AND GENESIS OF GARNET CRYSTALS IN THE METAMORPHIC AND IGNEOUS ROCKS IN THE HAMADAN AREA. IRANIAN JOURNAL OF GEOLOGY[Internet]. 2011;5(19):3-14. Available from: https://sid.ir/paper/129431/en

IEEE: Copy

ZAHRA HOSSEIN MIRZAEE, R. DADKHAH, and ZOHREH HOSSEIN MIRZAEE, “THE STUDY OF CHEMICAL COMPOSITION, ZONING AND GENESIS OF GARNET CRYSTALS IN THE METAMORPHIC AND IGNEOUS ROCKS IN THE HAMADAN AREA,” IRANIAN JOURNAL OF GEOLOGY, vol. 5, no. 19, pp. 3–14, 2011, [Online]. Available: https://sid.ir/paper/129431/en

Related Journal Papers