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A. Ahmadi Khalaji, Z. Tahmasbi and R. Zarei Sahamieh
Journal of Applied Sciences, 2009, 9(5), 843-853.
The Boroujerd pluton is chiefly constituted of quartz-diorite, granodiorite and monzogranite. The mineral chemistry and microprobe analysis of mineral assemblages in these rocks indicate that the magma in this area has a metaluminous to slightly peraluminous composition, related to calc-alkaline, arc-type magmas and displays features typical of I-type granitoids. Also, the average pressure and temperature is estimated at 1.093 ± 0.6 k bars and 785 ± 40 in quartz-diorites, respectively. All analyzed samples have log FO2-14.1 which show this magma crystallized in high oxygen fugacity. Also, the occurrence of magnesio-hornblende and Fe2+biotite in Boroujerd rocks suggest relatively oxidized magma.
ASCI-ID: 35-2855
Journal of Applied Sciences, 2009, 9(5), 874-882.
Thermobarometry of the Astaneh Pluton and its Related Subvolcanic Rocks (Sanandaj-Sirjan Zone, Western Iran)Journal of Applied Sciences, 2009, 9(5), 874-882.
Thermobarometry of the Astaneh Pluton and its Related Subvolcanic Rocks (Sanandaj-Sirjan Zone, Western Iran)Journal of Applied Sciences, 2009, 9(5), 874-882.
Ore Geology Reviews, 2019, 111(), 102849. DOI: 10.1016/j.oregeorev.2019.02.034
P – T – t path of the Boroujerd Complex, north‐west Sanandaj–Sirjan Zone, western Iran: Insights from phase equilibrium modelling and thermobarometryGeological Journal, 2021, 56(6), 3396. DOI: 10.1002/gj.4135
Petrogenesis of Dehsard felsic rocks in the southwest of Kerman, Iran: Inference for the evolution of Sanandaj-Sirjan zoneJournal of African Earth Sciences, 2020, 172(), 103978. DOI: 10.1016/j.jafrearsci.2020.103978
On the use of major and trace elements composition of pyroxene and amphibole in the genesis of Boroujerd quartz-dioriteIranian Journal of Crystallography and Mineralogy, 2020, 28(4), 1009. DOI: 10.52547/ijcm.28.4.1009