Field evidences, petrographic features and geochemical studies show that the garnet-muscovite granitoids of Boland Parchin area are S-type and they have sharp contact with the host rocks (metamorphic rocks). Granitoids of Boland Parchin contain minerals such as quartz, K-feldspars, plagioclase, biotite and Al-rich minerals (such as muscovite and garnet). Chemical composition of K-feldspars, pla...

biotite samples from different units of boroujerd granitoid complex (bgc) of the sanandaj-sirjan zone, western iran, have beenanalyzed by electron microprobe for major elements. biotite analyses from three units of quartzdiorite, granodiorite and monzograniteof bgc have their own distinct non-overlapping compositional fields in the annite – siderophyllite – phlogopite – eastonitequadrilateral (...

introduction the generation and evolution of granitic magmas has been a hot debated subject among petrologists. the diversity of their origin has led different authors to propose that these rocks are not simple in their origin and might be generated in more ways than one. in the past several decades, many petrologists used a variety characteristics to subdivide the granitoid rocks. such proposa...

Khetri Copper Belt, Rajasthan, is anthropogenically active and geologically belongs to the Delhi super-group. A study was designed understand geochemical processes controlling elemental mobility in groundwater. Sampling sites were divided into three zones, i.e. copper, quartzite granite mine zones depending on type of mineral excavated. total 32 representative groundwater samples collected anal...

Abstract Calculating the temperatures of magmas from which granitoid rocks solidify is a key task studying their petrogenesis, but few geothermometers are satisfactory. Zircon saturation thermometry has been most widely used because it conceptually simple and practically convenient, based on experimental calibrations with significant correlation calculated zircon temperature ( T Zr ) zirconium ...