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shakeri S. Mineralogy and type of iron ore generation in Abponeh mine, Sanandaj Sirjan zone. www.ijcm.ir 2024; 32 (2) :287-300
URL: http://ijcm.ir/article-1-1883-en.html
URL: http://ijcm.ir/article-1-1883-en.html
Department of Geology, Minerals and Water Resources, Faculty of Earth Sciences, Shahid Beheshti University, Tehran, Iran
Abstract: (589 Views)
Abpooneh iron mine is located 85 km west of Isfahan province in the middle part of Sanandaj-Sirjan structural zone. The host rock of Abpooneh ore are meta sandstone, schist and phyllite. Silicate minerals that were created during the metamorphosis of the host rock in the ore include muscovite, chlorite and indicate the green schist facies. Iron ore mainly show a banded and lumpy textures. In terms of texture, mineralogy and chemical composition, the iron ore is comparable to the metamorphosed iron ores. The textural and structural features is indicate the sedimentary-diagenetic origin of the ore in Abpooneh. Metamorphism occurred after the formation of the ore and caused the recrystallization of the ore and the host rock. The constituent components of the ore result of the erosion of continental destructive rocks and may have been provided by hydrothermal fluids related to submarine volcanic activities. The pattern of distribution of main and minor elements of ore and host rock is similar in various charts and this indicates their formation in a similar sedimentary environment.
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