اضافه کردن به علاقه‌مندی‌ها

محل انتشار

همایش بین المللی ژئولیت ایران

اطلاعات انتشار

سال

صفحات

۸ صفحه

کلمات کلیدی

Central Iran، Gandy Zeolite Mine، Na، clinoptilolite

The studied area has been located in the Moaleman area is situating in Torud Quadrangle in the north of
Central Iran. The Karaj Formation (Middle Eocene) with crops out from Reshm Village to Gandy Zeolite
Mine is observed in the north part of the studied area. In addition to the mentioned area, this zeolite has been
further exposed, extending to south and north of Semnan and then to Garmsar. According to the data, the
studied zeolite is Na–clinopetilolite and has paragenesis of opal, smectite clay, calcite and dolomite. The base
rock of this zeolite is rhyodacite trchyandesite and forming magmatic Seri is alkaline<\div>

راهنمای دریافت مقاله‌ی «Mineralogical specifications of the Gandy zeolite, east Moaleman north Central Iran» در حال تکمیل می‌باشد.

دریافت فایل PDF

۸۰۰۰ تومان

دریافت فایل Word + PDF

۱۱۰۰۰ تومان