MINERALOGY AND GEOCHEMISTRY OF SKARN FE OREBODY AND SYENODIORITIC INTRUSIVE HOST ROCK IN ZEBER KUH PROSPECT AREA (SW BARDASKAN, SOUTH KHORASAN PROVINCE)

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NAROOIE HOSSEIN; MALEKZADEH SHAFAROUDI AZADEH; KARIMPOUR MOHAMMAD HASSAN

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Journal: PETROLOGY Year:2017 | Volume:8 | Issue:31 Page(s): 89-110

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Title

MINERALOGY AND GEOCHEMISTRY OF SKARN FE OREBODY AND SYENODIORITIC INTRUSIVE HOST ROCK IN ZEBER KUH PROSPECT AREA (SW BARDASKAN, SOUTH KHORASAN PROVINCE)

Author(s)

NAROOIE HOSSEIN | MALEKZADEH SHAFAROUDI AZADEH | KARIMPOUR MOHAMMAD HASSAN | Issue Writer Certificate

Keywords

LOW TEMPERATURE FE SKARNQ1

MAGNETITEQ2

GEOCHEMISTRY OF INTRUSIVE ROCKQ1

ZEBER KUHQ1

KASHMAR-KERMAN TECTONIC ZONEQ1

Abstract

The ZEBER KUH prospect area is located southwest of Bardaskan, South Khorasan province, in the northeastern Iran. Lithologically, the area includes Rizu and Soltanieh Formations metamorphosed carbonate rocks, which were intruded by syenogranitic and syenodioritic intrusions. Field observations and laboratory studies such as structural controls of orebody, metasomatic replacement and formation of low temperature H2O-bearing minerals, and the occurrence of MAGNETITE and pyrite associated with chlorite, epidote, calcite, and quartz indicate that the iron mineralization is low temperature skarn-type. The source of Fe mineralization is probably a younger intrusive rock at depth. Hydrothermal ore fluid was ascended within fault zone and/or contact between the intrusive rock and the carbonate unit and generated orebody. Iron grade ranges from 54 to 65 wt.% and sulfur value is > 3 wt.%. MAGNETITE chemistry and Ti, V, Al, Mn, Ni, and Cr contents are similar to skarn deposit. Biotite syenodiorite host rock has hypidiomorphic granular texture and it consists of plagioclase, K-feldspar, biotite, and apatite minerals. Chemically, this intrusive rock is K-series alkaline type, which was generated in within plate zone. This magma is characterized by strong enrichment in LREE, LILE (Rb, Cs, Ba, and K), HFSE (Nb, Zr, and Ti), and P elements. The primary magma is produced by low degree partial melting of garnet lherzolite from asthenospheric to boundary of asthenospheric-lithospheric mantle.

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APA: Copy

NAROOIE, HOSSEIN, MALEKZADEH SHAFAROUDI, AZADEH, & KARIMPOUR, MOHAMMAD HASSAN. (2017). MINERALOGY AND GEOCHEMISTRY OF SKARN FE OREBODY AND SYENODIORITIC INTRUSIVE HOST ROCK IN ZEBER KUH PROSPECT AREA (SW BARDASKAN, SOUTH KHORASAN PROVINCE). PETROLOGY, 8(31 ), 89-110. SID. https://sid.ir/paper/197005/en

Vancouver: Copy

NAROOIE HOSSEIN, MALEKZADEH SHAFAROUDI AZADEH, KARIMPOUR MOHAMMAD HASSAN. MINERALOGY AND GEOCHEMISTRY OF SKARN FE OREBODY AND SYENODIORITIC INTRUSIVE HOST ROCK IN ZEBER KUH PROSPECT AREA (SW BARDASKAN, SOUTH KHORASAN PROVINCE). PETROLOGY[Internet]. 2017;8(31 ):89-110. Available from: https://sid.ir/paper/197005/en

IEEE: Copy

HOSSEIN NAROOIE, AZADEH MALEKZADEH SHAFAROUDI, and MOHAMMAD HASSAN KARIMPOUR, “MINERALOGY AND GEOCHEMISTRY OF SKARN FE OREBODY AND SYENODIORITIC INTRUSIVE HOST ROCK IN ZEBER KUH PROSPECT AREA (SW BARDASKAN, SOUTH KHORASAN PROVINCE),” PETROLOGY, vol. 8, no. 31 , pp. 89–110, 2017, [Online]. Available: https://sid.ir/paper/197005/en

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