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Home Â» Articles

Articles

Writers : Etemad Khah, Z.; Khatib, M. M.; Zarin Koob, M. H.
Refference : 28th Symposium on Geosciences and the 14th Symposium on Geological Society of Iran
Publishing Year : 1389

Abstract :

Tectonic genesis in south of Birjand affected compersional-sinestral shear zone with structural trend E-W. Sub volcanic rock unit with open spaces in this area of performance is consistent. Microscopic and mesoscopy evidences show deformation in the rock units and synkinematic during and after the emplacement of magma.  In this research, Mass Givshad sub volcanic deformation in during the development of magmatic fabrics and subsequent solid-state deformation fabrics were investigated.
XY elliptical strain in thin sections directional between N10°W to N30°W varies. General review microscopic and mesoscopy show coupling of tectonic between magma emplacement and tectonic regime.


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