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Information Journal Paper

Title

Mineral chemistry of the Permian basalts from North of Baladeh Central Alborz: Geothermobarometry and tectonomagmatic setting

Pages

  3-14

Abstract

 The Permian volcanic rocks of Central Alborz (northeast of Baladeh-Siahbisheh) crop out between Ruteh and Nesen Formations. The volcanic rocks are predominantly basaltic and plagioclase-phyric. Ferromagnesian minerals such as clinopyroxene and olivine are not modally abundant and sometimes are totally altered. Based on microprobe data, clinopyroxene and plagioclase are diopside (En34. 2-36. 4 Wo43. 1-47. 2 Fs14. 9-18. 1) and labradorite (50

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    APA: Copy

    ROSTAMI, F., DELAVARI, M., AMINI, S., & DOLATI, A.. (2018). Mineral chemistry of the Permian basalts from North of Baladeh Central Alborz: Geothermobarometry and tectonomagmatic setting. GEOSCIENCES, 27(106 ), 3-14. SID. https://sid.ir/paper/32090/en

    Vancouver: Copy

    ROSTAMI F., DELAVARI M., AMINI S., DOLATI A.. Mineral chemistry of the Permian basalts from North of Baladeh Central Alborz: Geothermobarometry and tectonomagmatic setting. GEOSCIENCES[Internet]. 2018;27(106 ):3-14. Available from: https://sid.ir/paper/32090/en

    IEEE: Copy

    F. ROSTAMI, M. DELAVARI, S. AMINI, and A. DOLATI, “Mineral chemistry of the Permian basalts from North of Baladeh Central Alborz: Geothermobarometry and tectonomagmatic setting,” GEOSCIENCES, vol. 27, no. 106 , pp. 3–14, 2018, [Online]. Available: https://sid.ir/paper/32090/en

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