Document Type : Original Research Paper

Authors

1 Ph.D. Student, Department of Earth Sciences, Faculty of Natural Sciences, University of Tabriz, Tabriz, Iran

2 Professor, Department of Earth Sciences, Faculty of Natural Sciences, University of Tabriz, Tabriz, Iran

3 Associate Professor, Faculty of Geology, University of Shahid Chamran, Ahvaz, Iran

Abstract

Calc-silicate hornfelses are resulted from temperature excreted from the Alvand Batholith on the surrounding carbonate rocks. Metamorphic minerals in these rocks are vesuvianite + garnet+clinopyroxene+ tremolite/actinolite+quartz+calcite±epidote. Calc- silicate minerals occurred in two stages of prograde and retrograde metamorphism. Mineral chemistry of clinopyroxene and garnet in calc-silicate hornfelses determined by EPMA shows that these minerals are mainly diopside and grossular. Based on clinopyroxene-garnet thermometry with coexisting minerals such as tremolite/actinolite, quartz, . . . temperature of ~550˚C was calculated for metamorphism of the clac-silicate hornfelses. Pressure of metamorphism was estimated to be about 3.5 Kbar. Fluid composition in the calc- silicate hornfelses had XCO2 = 0.2 which indicates that during prograde metamorphism carbonate minerals reacted out and the amount of these minerals was reduced in the rocks.

Keywords

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