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Title

PLAGIOCLASE AND BIOTITE MINERAL CHEMISTRY USED IN THE EVALUATION OF THE TEMPERATURE AND PRESSURE OF TORUD INTRUSIVE ASSOCIATION

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Abstract

 This paper elucidates the compositional studies on BIOTITEs and PLAGIOCLASEs in granitoid rocks of TORUD area to understand the geotectonic setting and geothermobarometry conditions. The TORUD granitoids with Oligocene age are composed of quartzmonzonite to granite. The main minerals of granitoids are quartz, PLAGIOCLASE, and K-feldspar. Other constituents are BIOTITE, amphibole, sphene and opaque minerals. Various textures including granular, myrmekitic, graphic, and prethite are observed in these rocks. According to the calculations of mineral PLAGIOCLASE thermometery in granitoid rocks, pressure was about 1.5 to 2.5 kbar and the temperature of crystallization have measured about 700 to 1000oC. Also, the compositions of BIOTITEs in intrusive bodies indicate that they are of magmatic origin with calc-alkaline affinities having formed in a tensional tectonic setting.

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    APA: Copy

    YAZDI, ABDOLLAH, SHAHHOSEINI, ELHAM, & AMIRI, ALI. (2014). PLAGIOCLASE AND BIOTITE MINERAL CHEMISTRY USED IN THE EVALUATION OF THE TEMPERATURE AND PRESSURE OF TORUD INTRUSIVE ASSOCIATION. GEOCHEMISTRY, 3(3), 0-0. SID. https://sid.ir/paper/394159/en

    Vancouver: Copy

    YAZDI ABDOLLAH, SHAHHOSEINI ELHAM, AMIRI ALI. PLAGIOCLASE AND BIOTITE MINERAL CHEMISTRY USED IN THE EVALUATION OF THE TEMPERATURE AND PRESSURE OF TORUD INTRUSIVE ASSOCIATION. GEOCHEMISTRY[Internet]. 2014;3(3):0-0. Available from: https://sid.ir/paper/394159/en

    IEEE: Copy

    ABDOLLAH YAZDI, ELHAM SHAHHOSEINI, and ALI AMIRI, “PLAGIOCLASE AND BIOTITE MINERAL CHEMISTRY USED IN THE EVALUATION OF THE TEMPERATURE AND PRESSURE OF TORUD INTRUSIVE ASSOCIATION,” GEOCHEMISTRY, vol. 3, no. 3, pp. 0–0, 2014, [Online]. Available: https://sid.ir/paper/394159/en

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