ZAGROS OROGEN: ZAGROS OROGENY AND THE NATURE OF DERIVATIVE GRANITOIDS IN CENTRAL SEGMENT OF SANANDAJ-SIRJAN ZONE, IRAN

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ESNA ASHARI AMIR; Peighambari Sima

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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: ZAGROS OROGENY AND THE NATURE OF DERIVATIVE GRANITOIDS IN CENTRAL SEGMENT OF SANANDAJ-SIRJAN ZONE, IRAN

Author(s)

ESNA ASHARI AMIR | Peighambari Sima

Keywords

Not Registered.

Abstract

SANDNDAJ-SIRJAN ZONE (SSZ) IS A SUBZONE OF THE ZAGROS OROGENIC BELT (ZOB) OF IRAN. ZOB RESULTED FROM THE ARABIAN–IRANIAN MICROPLATE CONTINENTAL COLLISION FOLLOWING THE SUBDUCTION OF THE NEOTETHYS OCEANIC CRUST UNDERNEATH IRAN (E.G. AGARD ET AL. 2011). SSZ MOSTLY CONSISTS OF A BASEMENT MADE OF LOW- TO HIGH-GRADE METASEDIMENTARY ROCKS INTRUDED BY FELSIC TO MAFIC BODIES SHOWING GEOCHEMICAL ARC AFFINITY (E.G. AHMADI KHALAJI ET AL. 2007).

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APA: Copy

ESNA ASHARI, AMIR, & Peighambari, Sima. (2013). ZAGROS OROGEN: ZAGROS OROGENY AND THE NATURE OF DERIVATIVE GRANITOIDS IN CENTRAL SEGMENT OF SANANDAJ-SIRJAN ZONE, IRAN. SYMPOSIUM OF GEOLOGICAL SOCIETY OF IRAN. SID. https://sid.ir/paper/921699/en

Vancouver: Copy

ESNA ASHARI AMIR, Peighambari Sima. ZAGROS OROGEN: ZAGROS OROGENY AND THE NATURE OF DERIVATIVE GRANITOIDS IN CENTRAL SEGMENT OF SANANDAJ-SIRJAN ZONE, IRAN. 2013. Available from: https://sid.ir/paper/921699/en

IEEE: Copy

AMIR ESNA ASHARI, and Sima Peighambari, “ZAGROS OROGEN: ZAGROS OROGENY AND THE NATURE OF DERIVATIVE GRANITOIDS IN CENTRAL SEGMENT OF SANANDAJ-SIRJAN ZONE, IRAN,” presented at the SYMPOSIUM OF GEOLOGICAL SOCIETY OF IRAN. 2013, [Online]. Available: https://sid.ir/paper/921699/en

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