شیمی کانی و بررسی نقش آلومینیوم کل بیوتیت برای تشخیص نوع کانی‌زایی در توده‌های نفوذی محور کرج-طالقان

The intrusive bodies of Karaj-Taleghan axis in Central Alborz constitute, intruded the pyroclastic rocks of Karaj Formation in the form of sill, lopolith, stock and plug with distict distribution. Based on microscopic studies, these bodies have similar lithological composition and include olivine gabbro, olivine monzodiorite, olivine monzonite, pyroxene monzonite with felsic dikes of syenite. The major minerals of these rocks are plagioclase, alkali feldspar, pyroxene, olivine and biotite. Biotite is one of the most prominent ferromagnesian mineral in the studied bodies. Compositionally, it is plotted between the field of annite and siderophylite. Most of these biotites are primarly magmatic and some are plotted in the field reequilibrated area. Based on the FeO*, MgO and Al2O3 binary and ternary diagrams, the studied biotites plot in the calc-alkaline orogenic field and crystallization temperature has been calculated between 640º to 770 ºC. Furthermore, the calculated pressure of biotite crystallization, based on Al barometer, is 0/27 to 2/58 KB (average1/06 KB). The total aluminum content of biotite in intrusive bodies at Karaj-Taleghan axis ranges from 2/25 to 3/01. Ziyaran plutonic complex shows good potential for iron-copper mineralization and Prachan and Shekarnab bodies show high potential for lead and zinc mineralization.