THE TAFTAN VOLCANIC ROCKS: IMPLICATION FOR THE ADAKITIC MAGMATISM OF THE MAKRAN MAGMATIC ARC

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DELAVARI MORTEZA; SHAKERI ATA

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Journal: QUATERNARY JOURNAL OF IRAN Year:2016 | Volume:2 | Issue:1 Page(s): 1-14

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Information Journal Paper

Title

THE TAFTAN VOLCANIC ROCKS: IMPLICATION FOR THE ADAKITIC MAGMATISM OF THE MAKRAN MAGMATIC ARC

Author(s)

DELAVARI MORTEZA | SHAKERI ATA | Issue Writer Certificate

Keywords

ADAKITICQ2

MAKRANQ1

SOUTHEASTERN IRANQ2

TATANQ2

VOLCANIC ROCKSQ2

Abstract

Taftan volcano, located in the SOUTHEASTERN IRAN, is one of the active volcanic centers of the MAKRAN magmatic arc during Neogene-Quaternary. The MAKRAN arc is an east-west trending Neogene- Quaternary volcanic edifice (Pang et al., 2014) lying in the north of the MAKRAN accretionary prism. Three major volcanic centers in the north of MAKRAN from west to east are the Bazman, Taftan and Koh-i-Sultan volcanoes, respectively, form a ca.300 km long magmatic arc.

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APA: Copy

DELAVARI, MORTEZA, & SHAKERI, ATA. (2016). THE TAFTAN VOLCANIC ROCKS: IMPLICATION FOR THE ADAKITIC MAGMATISM OF THE MAKRAN MAGMATIC ARC. QUATERNARY JOURNAL OF IRAN, 2(1), 1-14. SID. https://sid.ir/paper/255916/en

Vancouver: Copy

DELAVARI MORTEZA, SHAKERI ATA. THE TAFTAN VOLCANIC ROCKS: IMPLICATION FOR THE ADAKITIC MAGMATISM OF THE MAKRAN MAGMATIC ARC. QUATERNARY JOURNAL OF IRAN[Internet]. 2016;2(1):1-14. Available from: https://sid.ir/paper/255916/en

IEEE: Copy

MORTEZA DELAVARI, and ATA SHAKERI, “THE TAFTAN VOLCANIC ROCKS: IMPLICATION FOR THE ADAKITIC MAGMATISM OF THE MAKRAN MAGMATIC ARC,” QUATERNARY JOURNAL OF IRAN, vol. 2, no. 1, pp. 1–14, 2016, [Online]. Available: https://sid.ir/paper/255916/en

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