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Title

THE PETROGRAPHY AND GEOCHEMISTRY DIORITIC ROCKS OF KAMAR ZARD MOUNTAIN AREA (NORTH OF TORBATE HEYDARIYEH)

Pages

  257-267

Abstract

 The study area is located in 15km north of TORBATE HEYDARIYEH and belongs to the Central Iran Structural Zone. This area has a variety of lithological composition. The main igneous rocks are DIORITEs, with different mineralogies. These rocks consist of meta-diorites, sub-volcanic pyroxene DIORITEs, pyroxene DIORITEs and hornblende DIORITEs. Petrographical studies show that these rocks usually include plagioclase, hornblende, pyroxene (augite) and chlorite. The main texture of these rocks is hypidiomorphic granular. Based on the geochemical studies, DIORITEs show a tholeiite trend. The magmatic contamination processes have an significant role in the formation and evolution of these rocks. These studies also indicate that the rocks have formed in a volcanic arc setting.

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    APA: Copy

    TAGHAVI, ZAHRA, MAZAHERI, SEYED AHMAD, & KHODAMI, MAHNAZ. (2015). THE PETROGRAPHY AND GEOCHEMISTRY DIORITIC ROCKS OF KAMAR ZARD MOUNTAIN AREA (NORTH OF TORBATE HEYDARIYEH). GEOCHEMISTRY, 4(3), 257-267. SID. https://sid.ir/paper/230884/en

    Vancouver: Copy

    TAGHAVI ZAHRA, MAZAHERI SEYED AHMAD, KHODAMI MAHNAZ. THE PETROGRAPHY AND GEOCHEMISTRY DIORITIC ROCKS OF KAMAR ZARD MOUNTAIN AREA (NORTH OF TORBATE HEYDARIYEH). GEOCHEMISTRY[Internet]. 2015;4(3):257-267. Available from: https://sid.ir/paper/230884/en

    IEEE: Copy

    ZAHRA TAGHAVI, SEYED AHMAD MAZAHERI, and MAHNAZ KHODAMI, “THE PETROGRAPHY AND GEOCHEMISTRY DIORITIC ROCKS OF KAMAR ZARD MOUNTAIN AREA (NORTH OF TORBATE HEYDARIYEH),” GEOCHEMISTRY, vol. 4, no. 3, pp. 257–267, 2015, [Online]. Available: https://sid.ir/paper/230884/en

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