شماره ركورد كنفرانس :
3306
عنوان مقاله :
Analcime and Natrolite of South Shahr-e-Rey, North Central Iran
پديدآورندگان :
Bazargani-Guilani Kamaladdin Department of Geology, University of Tehran , Rabbani Mohammad Sadegh Department of Chemistry, University of Tehran , Youssefey Parisa Department of Geology, University of Tehran
كليدواژه :
Zeolite , Shahr-e-Rey , Central Iran
عنوان كنفرانس :
كنفرانس بين المللي زئوليت ايران
چكيده لاتين :
The minerals identified in the Sahr-e-Rey region, in order of their relative time of formations, are
primary calcite, tetranatrolite, analcime, natrolite, mesolite, stilbite, secondary calcite and quartz. The
formation of zeolites begins with a sodium zeolite of low Si/Al ratio content. They continue to form with
gradual increase of calcium and Si/Al ratio contents and terminate with secondary calcite or sometimes with
silica. There has been found some similarities between the sequence of formation of zeolites in amygdales
and veins of Shahr-e-Rey and Kuh-e-Aradeh. The analcime formula of the study region,
Na15.6Al15.2Si32.7O9610.6 H2O, shows that it has a hydrothermal origin