The mineralogical and petrological constraints of the Cretaceous Kermanshah ophiolitic complex in Nourabad and Dinavar regions in western Iran

Author:

Asiabanha Abbas,Bardintzeff Jacques-Marie,Shayegh Kobra

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference48 articles.

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2. Allahyari K, Saccani E, Pourmoafi M, Beccaluva L, Masoudi F (2010) Petrology of mantle peridotites and intrusive mafic rocks from the Kermanshah ophiolitic complex (Zagros belt, Iran): implications for the geodynamic evolution of the Neo-Tethyan oceanic branch between Arabia and Iran. Ofioliti 35:71–90

3. Ancey M, Bastenaire F, Tixier R (1977) Statistical control and optimization of X-ray intensity measurements. J Phys D: Appl Phys 10:817–830

4. Ancey M, Bastenaire F, Tixier R (1980) Application of statistical methods to electron probe microanalysis. In: Beaman DR, Ogilvie RE, Wittry DB (eds) Proceedings of the 8th International Congress on X-Ray optics and Microanalysis, Boston/MA 1977. Pendell Publishing Company, Midland/MI, p 49

5. Ao S, Xiao W, Khalatbari-Jafari M, Talebian M, Chen L, Wan B, Weiqiang J, Zhang Z (2016) U-Pb zircon ages, field geology and geochemistry of the Kermanshah ophiolite (Iran): from continental rifting at 79 Ma to oceanic core complex at ca. 36 Ma in the southern Neo-Tethys. Gondwana Res 31:305–318

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