Petrology and genesis of Vash granitoid NW Natanz (Isfahan)
Petrology and genesis of Vash granitoid NW Natanz (Isfahan)

Ali Khan Nasr Esfahani; Behafarin Shojaei

Volume 2, Issue 8 , January 2012, , Pages 99-114

Abstract
  The Vash granitoid is located in NW Natanz and is a part of Uromieh-Dokhtar magmatic belt in Central Iran. This pluton is probably of Oligo-Miocene age and is the result of extensive ...  Read More