ALBITIZATION IN IGNEOUS ROCKS OF CHAH- JULEH 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.

YAZDI M.; NOURIAN Z.; RASSA I.; BOSKABADI A.; KETABDARI M.

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

Journal Paper

Paper Information

Journal: JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY) Year:2011 | Volume:21 | Issue:81 (GEOLOGY ISSUE) Page(s): 125-140

Download Full-Text

Persian Verion

View:

1,036

Download:

Cites:

Information Journal Paper

Title

ALBITIZATION IN IGNEOUS ROCKS OF CHAH- JULEH AREA

Author(s)

Keywords

NA- METASOMATISMQ2

ZARIGAN LEUCOGRANITEQ2

CHAH-JULEHQ2

CENTRAL IRANQ2

Abstract

Introduction: Chah- Juleh area is located in 170 km NE of Yazd city and CENTRAL IRAN suture zone. The local geological setting consists up ZARIGAN LEUCOGRANITE, quartz diorite and diabasic dykes. ZARIGAN LEUCOGRANITE is the largest intrusive body by Early Camberian age in the study area.Aim: The main of the research was to confirm albitization, hematitization and U minerlization on the basis of field geology, petrography and geochemistry.Materials and Methods: In the research, we analyzed 63 samples by XRF, 11 samples by XRD in AEO laboratory. Also we used field geology and petrographic data of 23 thin sections.Results: Pseudomorph texture, albite replacing in orthose, heterogenous texture, and chess board texture of plagioclase, high Na2O and low SiO2 and K2O confirm the sodic-feric metasomatism in these rocks.Conclusion: According to petrological and geochemical data, ZARIGAN LEUCOGRANITE is I- type granites, sub- alkaline to calc- alkaline, volcanic arc type and ranging from leucogranite, quartz diorite to diabasic dykes. Infiltration of sodic solutions caused albitization and hematitization and U mineralization in the area.

Cites

No record.

References

No record.

Cite

APA: Copy

YAZDI, M., NOURIAN, Z., RASSA, I., BOSKABADI, A., & KETABDARI, M.. (2011). ALBITIZATION IN IGNEOUS ROCKS OF CHAH- JULEH AREA. JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY), 21(81 (GEOLOGY ISSUE)), 125-140. SID. https://sid.ir/paper/70262/en

Vancouver: Copy

YAZDI M., NOURIAN Z., RASSA I., BOSKABADI A., KETABDARI M.. ALBITIZATION IN IGNEOUS ROCKS OF CHAH- JULEH AREA. JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY)[Internet]. 2011;21(81 (GEOLOGY ISSUE)):125-140. Available from: https://sid.ir/paper/70262/en

IEEE: Copy

M. YAZDI, Z. NOURIAN, I. RASSA, A. BOSKABADI, and M. KETABDARI, “ALBITIZATION IN IGNEOUS ROCKS OF CHAH- JULEH AREA,” JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY), vol. 21, no. 81 (GEOLOGY ISSUE), pp. 125–140, 2011, [Online]. Available: https://sid.ir/paper/70262/en

Related Journal Papers