PETROLOGY AND GEOCHEMISTRY OF THE OUCH-PELANG GRANITOID, NORTHEASTERN KASHMAR

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.

ESMAEILI D.; RAZEGHI M.R.

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:2008 | Volume:34 | Issue:2 Page(s): 87-97

Download Full-Text

Persian Verion

View:

1,096

Download:

Cites:

Information Journal Paper

Title

PETROLOGY AND GEOCHEMISTRY OF THE OUCH-PELANG GRANITOID, NORTHEASTERN KASHMAR

Author(s)

ESMAEILI D. | RAZEGHI M.R. | Issue Writer Certificate

Keywords

I-TYPE GRANITEQ3

VOLCANIC ARCQ3

OUCH- PELANGQ3

CENTRAL IRANQ3

Abstract

The Tertiary Ouch-Pelang granitoid massif is located in the northeast of Kashmar city and tectonically belongs to the eastern CENTRAL IRAN zone. The massif has been cut the Eocene volcanic rocks and, based on the field study, mineralogy and geochemistry, is mainly composed of granodiorite, quartz-monzonite and monzonite with some granite. The rocks show granular, porphyroid and rarely mirmikitic textures. SiO2 display a small range (from 62% to 70%) and show a positive correlation with Fe2O3, MgO, MnO, TiO2, CaO, Al2O3, P2O5, Cr, V, Co, Ni, Pb and Nd and a negative correlation with K2O, U, Zr, Y, Th, and Yb and remains invariable against Na2O and Cs, Rb and Ba. The regular variation of the Harker diagram could be related to the fractional crystallization and the scattered patterns may relate to the assimilation. This massif is a metaluminous to slightly peraluminous and typical of I-TYPE GRANITEs. It belongs to high-K calk-alkaline series and displays geochemical characteristics typical of VOLCANIC ARC granites related to an active continental margin (e.g. a significant Nb, Ti, P and Sr depletion and K, Th, Rb and LREE restoration) which may perhaps connected to the subduction of the Neothethys under the CENTRAL IRAN.

Cites

No record.

References

ژئوشیمی، خاستگاه و پتانسیل کانی سازی طلا در منطقه اکتشافی کوه زر تربت حیدریه

Cite

APA: Copy

ESMAEILI, D., & RAZEGHI, M.R.. (2008). PETROLOGY AND GEOCHEMISTRY OF THE OUCH-PELANG GRANITOID, NORTHEASTERN KASHMAR. JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT), 34(2), 87-97. SID. https://sid.ir/paper/2205/en

Vancouver: Copy

ESMAEILI D., RAZEGHI M.R.. PETROLOGY AND GEOCHEMISTRY OF THE OUCH-PELANG GRANITOID, NORTHEASTERN KASHMAR. JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT)[Internet]. 2008;34(2):87-97. Available from: https://sid.ir/paper/2205/en

IEEE: Copy

D. ESMAEILI, and M.R. RAZEGHI, “PETROLOGY AND GEOCHEMISTRY OF THE OUCH-PELANG GRANITOID, NORTHEASTERN KASHMAR,” JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT), vol. 34, no. 2, pp. 87–97, 2008, [Online]. Available: https://sid.ir/paper/2205/en

Related Journal Papers