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مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

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Title

INVESTIGATION ON MINERALIZATION POTENTIAL OF MOLATALEB GRANITOID BODY USING GEOCHEMICAL CHARACTRISTICS

Pages

  158-165

Keywords

PBQ2
SNQ3

Abstract

 The MOLATALEB granitoid is located in the North West of Aligoudarz and at a distance of about 20 km of the Zagros Thrust Fault within the Sanandaj-Sirjan zone. It intruded into the Triassic and Jurassic metasediments during LARAMIDE orogeny. The intrusion has thermally metamorphosed the country rocks up to albite-epidote hornfels facies. Lithologically, the pluton is composed mainly of GRANITE and granodiorite of S-type. The granitoid plutons ocassionally show concentration of economic concentrations with special geochemical patterns. Geochemical investigation on MOLATALEB GRANITE, e.g., the quantities of Li and Ni in biotite, PB in K-feldspars and distribution of Mg/Li, K/Rb and Sr/Rb indicates that the MOLATALEB granitoid is barren with respect to economic elements.

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    APA: Copy

    BAGHERIAN, S., MOAZEN, M., DARVISHI, I., & KHAKZAD, A.. (2006). INVESTIGATION ON MINERALIZATION POTENTIAL OF MOLATALEB GRANITOID BODY USING GEOCHEMICAL CHARACTRISTICS. GEOSCIENCES, 15(58), 158-165. SID. https://sid.ir/paper/32593/en

    Vancouver: Copy

    BAGHERIAN S., MOAZEN M., DARVISHI I., KHAKZAD A.. INVESTIGATION ON MINERALIZATION POTENTIAL OF MOLATALEB GRANITOID BODY USING GEOCHEMICAL CHARACTRISTICS. GEOSCIENCES[Internet]. 2006;15(58):158-165. Available from: https://sid.ir/paper/32593/en

    IEEE: Copy

    S. BAGHERIAN, M. MOAZEN, I. DARVISHI, and A. KHAKZAD, “INVESTIGATION ON MINERALIZATION POTENTIAL OF MOLATALEB GRANITOID BODY USING GEOCHEMICAL CHARACTRISTICS,” GEOSCIENCES, vol. 15, no. 58, pp. 158–165, 2006, [Online]. Available: https://sid.ir/paper/32593/en

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