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
Tectonic and magmatic settings of the Oligocene felsic outcrops in the south of Ardestan, NE of Isfahan
Tectonic and magmatic settings of the Oligocene felsic outcrops in the south of Ardestan, NE of Isfahan

Ali Khan Nasr Esfahani; Babak Vahabi Mogadam

Volume 1, Issue 2 , September 2010, , Pages 95-108

Abstract
  The Oligocene felsic outcrops are located in the south of Ardestan (NE of Isfahan). The area is a part of Uromieh –Dokhtar structural zone. These outcrops are composed of ...  Read More