Persian
Home | News | Articles | Gallery | FAQ | Contact us | Sitemap | About us
Menu
Geology
Exploration
Geomatics
Chemistry lab
Geology Museum
geological maps
Main Projects
Finance & Official
Publication and Library
Articles
Thesises Index
Environment
Innovation and dehiscence year
uses of Geology
Geotourism
Quarterly Journal Geosciences Index
Geology of Khorassan
mines of Khorasan
book introduction
About us
services and products
Knowledges of Geology
The Eastern sun
Famous geoscientist of Iran
seminars
mashad
Geology and mine laws
Park Museum
Hot Links
Khorassan Geotourism
Khorassan's warm springs
GSINET project
Subsidence in Mashhad plate
Geology Museum
Home » Articles

Articles

Writers : Zafaranieh, A.; Noroozi, Gh. R.; Zia, H.; Jafari Poor Moghadam, E.
Refference : 28th Symposium on Geosciences and the 14th Symposium on Geological Society of Iran
Publishing Year : 1389

Abstract :

The region studied is located in Bisheh village in south Khorasan province, that is Nehbandan northeast. This region was considered for further investigations through the integration of results from geological, airborne geophysics, terrestrial geophysics and geochemical data and the knowledge concerning the obsolete mines. Identical airborne geophysics data from a distance of 15 kms from the region to be studied, after their interpretation and explanation together with the results from discovery excavations in the neighborhood have identified anomalies of iron. Within the region studied, the preliminary investigations were carried out by Magnetic method. The results from the geophysical processes showed the existence of magnetic anomalies in some parts of the region being studied. Thus, a region with an extent of 75 km2 was selected for further investigations. This paper has dealt with the submittal of the results from economic geology and petrographic studies. 50 thin sections were provided from this zone. The investigation of thin sections showed the existence of hematite and magnetite mineralization. In these sections, the minerals of iron were embedded into a matrix of sersite, chlorite and moscoite, and hematite was also formed in the cavities of rocks. These sections were also investigated in order to determine the alterations and, sersitic, carbonate, chloritic, propelitic, potassic and clayey alterations were identified and some details in regard to them have been submitted.


Subject List : , Altration

E-mail : info [at] gsinet [dot] ir
Last Update: 2010/09/26
Copyright © 2002-2007 GSINET , All rights reserverd.
P.B. : 91735-1166
18 Str. Sarafrazan Blv. Hour Sq., Mashhad - Iran
Tel: + 98 511 8218146-8 / Fax; +98 511 821 6044