Volume 11, Issue 1 (4-2003)                   www.ijcm.ir 2003, 11(1): 83-100 | Back to browse issues page

XML Persian Abstract Print

Download citation:
BibTeX | RIS | EndNote | Medlars | ProCite | Reference Manager | RefWorks
Send citation to:

Mineralogical and Geochemical characteristics of "Khezr-Abad pluton" NW of Taft, Iran.. www.ijcm.ir. 2003; 11 (1) :83-100
URL: http://ijcm.ir/article-1-778-en.html
Abstract:   (2924 Views)
Khezr-Abad pluton is cropped out in North-West of Taft. This granitoid seems to be younger than the surrounding metamorphosed rocks, particularly the lower cretaceous limestones and probably is implaced during Oligo-Miocene. The most volumetric abundances of the igneous rocks are:

granodiorite, granite, quartzmonzo-diorite, quartz-diorite, and in a lesser amount tonalite, quartz-syenite and syenite. All granitoid rocks show Ba, K, Rb enrichment, and Nb, Sr, Ti depletion.

From the economical potential point of view, mineralization of marble, Fe-Cu-Pb-Zn skarn and non-metalic minerals such as kaolinite are considerable.

Geothermobarometry of rock forming minerals of this pluton indicates temperature of  810- 985 ˚C and pressures of  2.43 – 6.2 kilobars (kbar).

Full-Text [PDF 121 kb]   (741 Downloads)    
Type of Study: Research | Subject: Special

Add your comments about this article : Your username or Email:

Rights and permissions
Creative Commons License This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.

© 2021 CC BY-NC 4.0 | Iranian Journal of Crystallography and Mineralogy

Designed & Developed by : Yektaweb