THE BEHAVIOR OF MAJOR AND TRACE ELEMENTS OF THE TOURMALINE FROM THE MANGAVAI AND GANJNAMEH PEGMATITIC ROCKS (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.

AHMADI KHALAJI AHMAD; TAHMASBI ZAHRA; ZAL FARHAD; SHABANI ZAHRA

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

Journal Paper

Paper Information

Journal: PETROLOGY Year:2016 | Volume:7 | Issue:27 Page(s): 1-24

Download Full-Text

Persian Verion

View:

636

Download:

Cites:

Information Journal Paper

Title

THE BEHAVIOR OF MAJOR AND TRACE ELEMENTS OF THE TOURMALINE FROM THE MANGAVAI AND GANJNAMEH PEGMATITIC ROCKS (HAMADAN AREA)

Author(s)

AHMADI KHALAJI AHMAD | TAHMASBI ZAHRA | ZAL FARHAD | SHABANI ZAHRA | Issue Writer Certificate

Keywords

SCHORLQ2

FOITITEQ1

OLENITEQ1

ZONINGQ1

MANGAVIQ1

GANJNAMEHQ2

ALVANDQ2

HAMEDANQ2

Abstract

The Mangavai and GANJNAMEH pegmatitic rocks are part of the ALVAND granitoid pluton in the Sanandaj-Sirjan zone. The composition of tourmaline in MANGAVI is SCHORL and that of the GANJNAMEH lies in the SCHORL- FOITITE fields. The amounts of aluminum and X-vacancy in the GANJNAMEH tourmalines are more than those of MANGAVI. But commonly, the main substitution of both types of tourmaline is proton production and Al increase types that Al increase; X-vacancy and Fe reduce occurred. During these substitutions, OLENITE and FOITITE, Al-tourmaline and X-vacancy have been formed, respectively. The absence of dravite and the Fe # value over 0.8 in analyzed samples indicate that the tourmalines in pegmatites are related to magmatic types. In addition, the substitution of X-vacancy and Na+Al (olenite) type of tourmaline point to its magmatic nature and so, the required elements (i.e. boron, iron, sodium and aluminum) provided by magmatic fluids. The HREE amount of the MANGAVI tourmalines due to accompanied garnet are very low but in the absence of garnet, the GANJNAMEH tourmaline have high levels of these elements. Although tourmalines have the extensive substitutions but do not have a tendency to absorb all rare earth elements and the greatest impact on the control of these elements in tourmaline related to paragenesis minerals.

Cites

No record.

References

No record.

Cite

APA: Copy

AHMADI KHALAJI, AHMAD, TAHMASBI, ZAHRA, ZAL, FARHAD, & SHABANI, ZAHRA. (2016). THE BEHAVIOR OF MAJOR AND TRACE ELEMENTS OF THE TOURMALINE FROM THE MANGAVAI AND GANJNAMEH PEGMATITIC ROCKS (HAMADAN AREA). PETROLOGY, 7(27 ), 1-24. SID. https://sid.ir/paper/197069/en

Vancouver: Copy

AHMADI KHALAJI AHMAD, TAHMASBI ZAHRA, ZAL FARHAD, SHABANI ZAHRA. THE BEHAVIOR OF MAJOR AND TRACE ELEMENTS OF THE TOURMALINE FROM THE MANGAVAI AND GANJNAMEH PEGMATITIC ROCKS (HAMADAN AREA). PETROLOGY[Internet]. 2016;7(27 ):1-24. Available from: https://sid.ir/paper/197069/en

IEEE: Copy

AHMAD AHMADI KHALAJI, ZAHRA TAHMASBI, FARHAD ZAL, and ZAHRA SHABANI, “THE BEHAVIOR OF MAJOR AND TRACE ELEMENTS OF THE TOURMALINE FROM THE MANGAVAI AND GANJNAMEH PEGMATITIC ROCKS (HAMADAN AREA),” PETROLOGY, vol. 7, no. 27 , pp. 1–24, 2016, [Online]. Available: https://sid.ir/paper/197069/en

Related Journal Papers