ZAGROS OROGEN: JURASSIC TO CENOZOIC TECTONICS OF THE ZAGROS OROGEN IN NORTHWESTERN IRAN

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MOHAJJEL M.; FERGUSSON C.L.

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Seminar Paper

Paper Information

Seminar: SYMPOSIUM OF GEOLOGICAL SOCIETY OF IRAN
Year:2013 | Issue:17

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Title

ZAGROS OROGEN: JURASSIC TO CENOZOIC TECTONICS OF THE ZAGROS OROGEN IN NORTHWESTERN IRAN

Author(s)

MOHAJJEL M. | FERGUSSON C.L.

Keywords

CONTINENTAL COLLISION

NORTHWESTERN IRAN

SANANDAJ–SIRJAN ZONE

SUBDUCTION

ZAGROS OROGEN

Abstract

THE ZAGROS MOUNTAINS OF IRAN FORMED BY CONTINENTAL COLLISION FROM CLOSURE OF THE NEO-TETHYAN OCEAN. NEW MAPPING, RADIOMETRIC AGES AND STRATIGRAPHIC ANALYSES HAVE ENABLED ADVANCES IN OUR UNDERSTANDING OF THE JURASSIC TO CENOZOIC TECTONIC HISTORY. THE NORTHWESTERN ZAGROS OROGEN CONSISTS OF THREE BELTS: (1) THE ZAGROS FOLD AND THRUST BELT, DIVIDED INTO THE OUTER ZAGROS SIMPLY FOLDED BELT AND THE INNER HIGH ZAGROS BELT, (2) THE ZAGROS SUTURE ZONE INCLUDING RADIOLARITE, OPHIOLITE AND BISOTUN LIMESTONE THRUST SHEETS, AND (3) THE SANANDAJ–SIRJAN ZONE, WHICH CONTAINS ABUNDANT METAMORPHIC ROCKS. ...

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APA: Copy

MOHAJJEL, M., & FERGUSSON, C.L.. (2013). ZAGROS OROGEN: JURASSIC TO CENOZOIC TECTONICS OF THE ZAGROS OROGEN IN NORTHWESTERN IRAN. SYMPOSIUM OF GEOLOGICAL SOCIETY OF IRAN. SID. https://sid.ir/paper/921696/en

Vancouver: Copy

MOHAJJEL M., FERGUSSON C.L.. ZAGROS OROGEN: JURASSIC TO CENOZOIC TECTONICS OF THE ZAGROS OROGEN IN NORTHWESTERN IRAN. 2013. Available from: https://sid.ir/paper/921696/en

IEEE: Copy

M. MOHAJJEL, and C.L. FERGUSSON, “ZAGROS OROGEN: JURASSIC TO CENOZOIC TECTONICS OF THE ZAGROS OROGEN IN NORTHWESTERN IRAN,” presented at the SYMPOSIUM OF GEOLOGICAL SOCIETY OF IRAN. 2013, [Online]. Available: https://sid.ir/paper/921696/en

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