Contribution of ultramafic rocks in central Sanandaj-Sirjan zone to the characterizing of physio-chemical condition during initiation of subduction
Contribution of ultramafic rocks in central Sanandaj-Sirjan zone to the characterizing of physio-chemical condition during initiation of subduction

Amir Esna-Ashari; Fatemeh Sarjoughian

Volume 8, Issue 32 , March 2018, , Pages 45-66

https://doi.org/10.22108/ijp.2017.100430.0

Abstract
  In the central part of the Sanandaj-Sirjan zone, there is an ultramafic rock exposure (hornblendite and pyroxenite) adjacent to Molataleb felsic complex completely located between Azna ...  Read More
Different geodynamic settings for Sistan suture zone ophiolitic units: discussion of textural evidences and mineral chemistry of crustal sequence ultramafic-mafic associations
Different geodynamic settings for Sistan suture zone ophiolitic units: discussion of textural evidences and mineral chemistry of crustal sequence ultramafic-mafic associations

Morteza Delavari

Volume 4, Issue 16 , February 2014, , Pages 39-58

Abstract
  Sistan suture zone ophiolitic rocks are remnants of Tethyan oceanic lithosphere between Lut and Afghan continental blocks. This oceanic basin has been existed at least during the Cretaceous. ...  Read More
Geochemistry, petrology and U-Pb geochronology of Ghazan mafic-ultramafic intrusion, NW Iran
Geochemistry, petrology and U-Pb geochronology of Ghazan mafic-ultramafic intrusion, NW Iran

Manijeh Asadpour; Seyed Mohammad Pourmoafi; Soraya Heuss

Volume 4, Issue 14 , July 2013, , Pages 1-16

Abstract
  Ghazan mafic-ultramafic intrusive is a small igneous body at the extremity of NW of Sanandaj-Sirjan zone in the NW of Iran, intruded into the early Paleozoic sedimentary rocks. This ...  Read More