TOURMALINIZATION IN THE ASTANEH GRANITOIDS (SOUTH WEST ARAK)

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.

TAHMASBI Z.; AHMADI KHALAJI A.; RAJAEIEH M.

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

Journal Paper

Paper Information

Journal: Iranian Journal of Crystallography and Mineralogy Year:2009 | Volume:17 | Issue:3 Page(s): 369-380

Download Full-Text

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

Persian Verion

View:

1,005

Download:

Cites:

Information Journal Paper

Title

TOURMALINIZATION IN THE ASTANEH GRANITOIDS (SOUTH WEST ARAK)

Author(s)

TAHMASBI Z. | AHMADI KHALAJI A. | RAJAEIEH M. | Issue Writer Certificate

Keywords

ASTANEHQ3

MICROPROBEQ3

METASOMATISMQ2

SANANDAJ- SIRJAN ZONEQ3

TOURMALINEQ2

Abstract

The studied area is a small portion of Sanandaj – Sirjan zone. METASOMATISM at the contact of intrusive body studied and penetration of Al-rich rocks caused tourmalinization to stratiform tourmalinite in pelitic hornfels. In addition, hydrothermal fluids crystallized TOURMALINE nodules in monzogranite surface. The Fe/ (Fe+Mg) ratio in varied between 0.4-0.76 in stratiform TOURMALINE and 0.83-0.96 in TOURMALINE nodules respectively. The TOURMALINE composition is schorlite- dravite. Chemical zoning in this mineral show that system is open and crystallization is unequilibrium. The flat trace end rare earth elements imply to mobility of LREE induced to alteration that this phenomena occur to increasing HREE/ LREE in this type TOURMALINEs.

Cites

References

No record.

Cite

APA: Copy

TAHMASBI, Z., AHMADI KHALAJI, A., & RAJAEIEH, M.. (2009). TOURMALINIZATION IN THE ASTANEH GRANITOIDS (SOUTH WEST ARAK). IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 17(3), 369-380. SID. https://sid.ir/paper/4183/en

Vancouver: Copy

TAHMASBI Z., AHMADI KHALAJI A., RAJAEIEH M.. TOURMALINIZATION IN THE ASTANEH GRANITOIDS (SOUTH WEST ARAK). IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2009;17(3):369-380. Available from: https://sid.ir/paper/4183/en

IEEE: Copy

Z. TAHMASBI, A. AHMADI KHALAJI, and M. RAJAEIEH, “TOURMALINIZATION IN THE ASTANEH GRANITOIDS (SOUTH WEST ARAK),” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 17, no. 3, pp. 369–380, 2009, [Online]. Available: https://sid.ir/paper/4183/en

Related Journal Papers