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Information Journal Paper

Title

INVESTIGATION OF NICKEL SULFIDE MINERALIZATION IN FARYAB AREA

Pages

  29-36

Abstract

 Platinum-Group elements (PGE) deposits often found with layered mafic–ultramafic association and PGE enrichments occur in Cu and Ni-rich SULFIDE MINERALIZATION. FARYAB OPHIOLITE area is the main resources of chromite in south of Iran that has SULFIDE MINERALIZATION in different lithology. Sulfide phases recognized by Microscopic methods. It indicates that main sulfides are including pyrrhotite, pentlandite, millerite and heazlewoodite. Samples are analyzed by ICP-MS, XRf and Atomic absortion. Results indicate that NICKEL SULFIDE MINERALIZATION has occurred.

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  • Cite

    APA: Copy

    PAZAND, K., & GHANBARI, YOUSEF. (2009). INVESTIGATION OF NICKEL SULFIDE MINERALIZATION IN FARYAB AREA. JOURNAL OF EARTH AND RESOURCES, 1(3), 29-36. SID. https://sid.ir/paper/164287/en

    Vancouver: Copy

    PAZAND K., GHANBARI YOUSEF. INVESTIGATION OF NICKEL SULFIDE MINERALIZATION IN FARYAB AREA. JOURNAL OF EARTH AND RESOURCES[Internet]. 2009;1(3):29-36. Available from: https://sid.ir/paper/164287/en

    IEEE: Copy

    K. PAZAND, and YOUSEF GHANBARI, “INVESTIGATION OF NICKEL SULFIDE MINERALIZATION IN FARYAB AREA,” JOURNAL OF EARTH AND RESOURCES, vol. 1, no. 3, pp. 29–36, 2009, [Online]. Available: https://sid.ir/paper/164287/en

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