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Title

MINERALOGY, STRUCTURAL AND TEXTURAL STUDIES AND GENESIS OF KHOSROW-ABAD IRON DEPOSIT, NE KERMANSHAH

Pages

  110-119

Abstract

 Khosrow-Abad iron deposit is located in the northeast of Kermanshah in Sanandaj-Sirjan geotectonic zone. Theunits outcropped in the area are the (iron-rich) andesitic volcanicsat the lower part of the sequence overlaying limestone. The aforementioned complex by the name of Songhor volcanosedimentarycomplex has been metamorphosed up to greenschist facies. Iron rich andesiteand limestone-units have been intruded by a granitic body led to a contact metamorphism and subsequent alteration by hydrothennal fluids, extracting iron from basaltic andesite and deposited it in the limestone adjacent to basaltic andesite and at the contact of granite. Iron occurrence confined to the contact of granite in carbonate and existence of skarn mineralogy support the occurrence of an iron skam deposit, but detailed studies on textures and structures suggest the source of the iron from the volcanosedimentarycomplex and its basaltic andesites.

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    APA: Copy

    MOTEVALI, K., GHADERI, M., & RASHIDNEZHAD OMRAN, N.A.. (2006). MINERALOGY, STRUCTURAL AND TEXTURAL STUDIES AND GENESIS OF KHOSROW-ABAD IRON DEPOSIT, NE KERMANSHAH. GEOSCIENCES, 15(60), 110-119. SID. https://sid.ir/paper/31469/en

    Vancouver: Copy

    MOTEVALI K., GHADERI M., RASHIDNEZHAD OMRAN N.A.. MINERALOGY, STRUCTURAL AND TEXTURAL STUDIES AND GENESIS OF KHOSROW-ABAD IRON DEPOSIT, NE KERMANSHAH. GEOSCIENCES[Internet]. 2006;15(60):110-119. Available from: https://sid.ir/paper/31469/en

    IEEE: Copy

    K. MOTEVALI, M. GHADERI, and N.A. RASHIDNEZHAD OMRAN, “MINERALOGY, STRUCTURAL AND TEXTURAL STUDIES AND GENESIS OF KHOSROW-ABAD IRON DEPOSIT, NE KERMANSHAH,” GEOSCIENCES, vol. 15, no. 60, pp. 110–119, 2006, [Online]. Available: https://sid.ir/paper/31469/en

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