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Information Journal Paper

Title

GEOCHEMISTRY AND ELEMENTAL VARIATIONS IN RAZI ABAD PORPHYRY COPPER MINERALIZATION, NORTHWEST OF JIROFT

Pages

  90-104

Abstract

 Razi Abad copper index locating in UROMIEH-DOKHTAR volcano-plutonic belt has Oligo-Miocene intrusive igneous and Eocene volcano-sedimentary rocks. The index is situated 25km northwest of Jiroft Township. Accessing to the area is possible via Kerman-Jiroft road. Surrounding rock units of RAZI ABAD mineralization are dark beds of shale, volcano-sedimentary units, Eocene andesitic lava, and granular quartz diorite intrusive units. On the other hand, host rocks of the mineralization are Oligo-Miocene subvolcanic units having micro-diorite, micro quartz diorite, porphyritic quartz monzodiorite, and porphyritic granodiorite compositions. Too many acidic, intermediate, and basic dykes are observed in intrusive rocks. Potassic, potassic-phyllic, phyllic, phyllic-argillic, quartz-pyrite, propylitic, and argillic alterations with various intensities have occurred in the study area. Potassic, potassic-phyllic, and phyllic alteration zones contain mineralization.Finally, by considering ENRICHMENTs and DEPLETIONs of major, minor, and trace elements in the host rocks of the mineralization, several alteration stages are recognized for the area. Correlation between supraore and subore elements such as zinc and copper implies telescopic shape of the mineralization, which has formed during at least two high- and low-temperature phases. Thus, dominant source of the mineralization and hydrothermal fluids could be a hidden intrusion with porphyritic granodiorite unit. Primary mineralization has occurred by high-temperature fluids in porphyritic micro-diorite rocks and then it has happened in porphyritic granodiorite stocks. The latter phase has affected on pre-existing alteration and mineralization zones. Therefore, porphyritic micro-diorite rocks have undergone several alteration phases and it seems that the primary mineralization has become enriched during next stages.

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    Cite

    APA: Copy

    TAYEBI, F., BEHZADI, M., RABEE, A., & EMAMI, M.H.. (2010). GEOCHEMISTRY AND ELEMENTAL VARIATIONS IN RAZI ABAD PORPHYRY COPPER MINERALIZATION, NORTHWEST OF JIROFT. RESEARCHES IN EARTH SCIENCES, 1(3), 90-104. SID. https://sid.ir/paper/207458/en

    Vancouver: Copy

    TAYEBI F., BEHZADI M., RABEE A., EMAMI M.H.. GEOCHEMISTRY AND ELEMENTAL VARIATIONS IN RAZI ABAD PORPHYRY COPPER MINERALIZATION, NORTHWEST OF JIROFT. RESEARCHES IN EARTH SCIENCES[Internet]. 2010;1(3):90-104. Available from: https://sid.ir/paper/207458/en

    IEEE: Copy

    F. TAYEBI, M. BEHZADI, A. RABEE, and M.H. EMAMI, “GEOCHEMISTRY AND ELEMENTAL VARIATIONS IN RAZI ABAD PORPHYRY COPPER MINERALIZATION, NORTHWEST OF JIROFT,” RESEARCHES IN EARTH SCIENCES, vol. 1, no. 3, pp. 90–104, 2010, [Online]. Available: https://sid.ir/paper/207458/en

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