Refference : 2nd National Symposium of Iranian Society of Economic Geology
Publishing Year : 1390

Abstract :

The Baharestan Kaolin Mine as a one of the mines of The plutonic- volcanic belt ,on the sothwest of Sabzevar Zone that occurs by intruded of the Oligomiocene massive (Honrblan quartz monzzonit porphyry, Monzonit porphyry) into Eocene calck-alkaline volcanic rocks (Dasiet, latite, H onbland andesite, Quartz honbland andesitez) and affected of its hydrothermal fluids. Structural studies showed that the pattern of regional structure, associated with left-slip structural shear zones that fram the main of Baharestan left-slip fault. Generally, the results of this study indicate that adoption of hydrothermal fluids associated with intrusion of the masses with kaolin mineralizationin the Damage zone of the the name Linkin Damage zone has been established.

Subject List : Kaolin