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Information Journal Paper

Title

GEOTHERMOMETERY OF HYDROTHERMAL ALTERATION ZONES BY CHLORITE THERMOMETERY AND COMPARED WITH FLUID INCLUSION GEOTHERMOMETERY

Pages

  12-20

Abstract

 Temperature determination of formation of hydrothermal or deposites and related ALTERATION ZONE is an important prospecting tool. Geothermometery, using secondary CHLORITE is a suitable method for indicting temperature for different types of alteration.Application of this method to ALTERATION ZONE in NW Zanjan, east of Mianeh and south of Khalkhal, gives temperatures of 340-365oC, 330-355oC, 315-325oC and 290-305oC for the sericitic, advanced argillic, moderate argillic, propylitic zone prospectively.Studied CHLORITE is repidolite. Estimation of temperature based on fluid inclusion studies are in good agreement with temperature obtained from CHLORITE thermometry. Therefore application of both of these methods is suggested for temperature estimation.

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    Cite

    APA: Copy

    HAJALILOU, B., & KHAKZAD, A.. (2007). GEOTHERMOMETERY OF HYDROTHERMAL ALTERATION ZONES BY CHLORITE THERMOMETERY AND COMPARED WITH FLUID INCLUSION GEOTHERMOMETERY. PEYKE NOOR JOURNAL SCIENCE, 1(2), 12-20. SID. https://sid.ir/paper/203502/en

    Vancouver: Copy

    HAJALILOU B., KHAKZAD A.. GEOTHERMOMETERY OF HYDROTHERMAL ALTERATION ZONES BY CHLORITE THERMOMETERY AND COMPARED WITH FLUID INCLUSION GEOTHERMOMETERY. PEYKE NOOR JOURNAL SCIENCE[Internet]. 2007;1(2):12-20. Available from: https://sid.ir/paper/203502/en

    IEEE: Copy

    B. HAJALILOU, and A. KHAKZAD, “GEOTHERMOMETERY OF HYDROTHERMAL ALTERATION ZONES BY CHLORITE THERMOMETERY AND COMPARED WITH FLUID INCLUSION GEOTHERMOMETERY,” PEYKE NOOR JOURNAL SCIENCE, vol. 1, no. 2, pp. 12–20, 2007, [Online]. Available: https://sid.ir/paper/203502/en

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