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Information Journal Paper

Title

PETROLOGY AND GEOCHEMISTRY OF AKAPOL GRANITOID (SW KELARDASHT, N IRAN)

Pages

  221-234

Abstract

 Akapol GRANITOID is located in the south-west of Kelardasht and is counted of plutonic massive in central ALBORZ zone. This plutonic massive with the age of about 54±4 to 56±3 Ma intruded in to the Formations of Mobarak and Shemshak and due to petrology, is containing syenodiorite, monzonite quartzmonzonite, granodiorite and monzogranite. The under-study samples have meta-aluminus and high K-Calk alkaline characteristics. Multi-element spider diagram of these samples shows lacking of Ti, Tb, Y, Tm, Yb and richness of K, Rb, Ba, Tb.These features show subduction related magmatism. Petrographic evidences which are presented in the monzogranite unit of AKAPOL, contain the partial absorbtion of plagioclases phenochryst, formation sieve texture in the plagioclases, presence of poikilitic texture, rapakivi and antirapakivi texture, as well as presence of microgranular enclaves and reactive margin between enclaves along with rounding stone and also presence of needle apatites, showing that magma mixing is an essential factor in the petrology of AKAPOL GRANITOID.

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    APA: Copy

    ESMAEILI, DARYOUSH, KHALAJ, MARZIEH, & VALIZADEH, M.V.. (2006). PETROLOGY AND GEOCHEMISTRY OF AKAPOL GRANITOID (SW KELARDASHT, N IRAN). JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT), 32(3 (SECTION GEOLOGY 2)), 221-234. SID. https://sid.ir/paper/2296/en

    Vancouver: Copy

    ESMAEILI DARYOUSH, KHALAJ MARZIEH, VALIZADEH M.V.. PETROLOGY AND GEOCHEMISTRY OF AKAPOL GRANITOID (SW KELARDASHT, N IRAN). JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT)[Internet]. 2006;32(3 (SECTION GEOLOGY 2)):221-234. Available from: https://sid.ir/paper/2296/en

    IEEE: Copy

    DARYOUSH ESMAEILI, MARZIEH KHALAJ, and M.V. VALIZADEH, “PETROLOGY AND GEOCHEMISTRY OF AKAPOL GRANITOID (SW KELARDASHT, N IRAN),” JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT), vol. 32, no. 3 (SECTION GEOLOGY 2), pp. 221–234, 2006, [Online]. Available: https://sid.ir/paper/2296/en

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