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Information Journal Paper

Title

INVESTIGATIONS ON COEXISTENCE OF ZOISITE- CLINOZOISITE IN METAMORPHIC ROCKS; AN EXAMPLE FROM SALMAS EPIDOTE- AMPHIBOLITES- NW OF IRAN

Pages

  27-36

Abstract

 Zoisite and clinozoisite are coexistent in the SALMAS EPIDOTE- AMPHIBOLITES, NW Iran.The frequency of zoisite is higher than clinozoisite in the studied EPIDOTE- AMPHIBOLITES. The pistacite content of zoisite is lower than clinozoisite. XPs in zoisite is about 6.46-10.65% while for clinozoisite it is about 16.72-18.73%. Al-Fe3+ substitution was effective to create the mineral compositional changes in the SALMAS epidote group minerals. Composition of coexisting zoisite and clinozoisite is a function of pressure, temperature and whole rock composition. According to zoisite and clinozoisite phase relations and compositions, epidote- amphibolite metamorphism in the SALMAS area occurred at temperature of 500±20 oC and pressure of 6.5-7 Kbar conditions.

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    APA: Copy

    AHANGARI, M., & MOAZZEN, M.. (2014). INVESTIGATIONS ON COEXISTENCE OF ZOISITE- CLINOZOISITE IN METAMORPHIC ROCKS; AN EXAMPLE FROM SALMAS EPIDOTE- AMPHIBOLITES- NW OF IRAN. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 22(1), 27-36. SID. https://sid.ir/paper/4265/en

    Vancouver: Copy

    AHANGARI M., MOAZZEN M.. INVESTIGATIONS ON COEXISTENCE OF ZOISITE- CLINOZOISITE IN METAMORPHIC ROCKS; AN EXAMPLE FROM SALMAS EPIDOTE- AMPHIBOLITES- NW OF IRAN. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2014;22(1):27-36. Available from: https://sid.ir/paper/4265/en

    IEEE: Copy

    M. AHANGARI, and M. MOAZZEN, “INVESTIGATIONS ON COEXISTENCE OF ZOISITE- CLINOZOISITE IN METAMORPHIC ROCKS; AN EXAMPLE FROM SALMAS EPIDOTE- AMPHIBOLITES- NW OF IRAN,” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 22, no. 1, pp. 27–36, 2014, [Online]. Available: https://sid.ir/paper/4265/en

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