chemical characteristics of biotite from boroujerd granitoid complex (middle jurassic), western iran

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 (aspe), reflecting their host rock compositions. biotite from each rock unit has an increasing trend of al contents atalmost fixed fe/(fe+mg) values. in quartzdiorite it shows an approximately constant range of fe/(fe+mg) with a low to moderate alcontent from 2.5 to 3 atoms per formula unit (apfu). biotite from granodiorite exhibits a fairly wide range of al values reaching up to3.32 apfu, at fe/(fe+mg) from 0.6 to 0.7, whereas biotite from monzogranite have a relatively narrow range of fe/(fe+mg) and totalal values of limited range of 3.1 to 3.3 apfu. biotite compositions from these two latter units considered to be derived entirely fromcrustal material, characterized by a remarkable increase in total al at relatively high fe contents. biotite samples of quartzdioritesdefine a distinct and non-overlapping trend from those of granidiorites and monzogranites and hence interpreted to be derived from aparental magma with different composition. calculation of log(xmg/xfe) ranges from -0.09 to -0.02 and most of samples fromquartzdiorite fall within weakly and moderately contaminated i-type field of log(xf/xoh) versus log(xmg/xfe) diagram, whereasthe other two units, containing biotites with log(xmg/ xfe)< -0.21, classified as strongly contaminated reduced i-type. oxygenfugacity (log ƒo2) of -15.4 to -17.5 bars and ƒh2o of 200 to 560 bars were calculated for quartzdiorite. likewise, log (ƒo2) of –17.66bars and water fugacity (ƒh2o) of 400 and 700 bars were also calculated for granodiorite and monzogranites respectively. in thefeo*–mgo–al2o3 biotite discrimination diagram, biotite compositions from bgc are distributed between the calc-alkaline andperaluminous fields, i.e., biotite from the qaurtzdioritic rocks fall principally in the calc-alkaline field, whereas those from thegranodioritic and monzogranitic units plot almost exclusively in the peraluminous field consistent with their host rock nature