Writers : Moosavi, S. M.; Alavi, S. A.; Khatib, M. M.
Refference : The Forth National Geological Conference of Payam Noor University(PNU)
Publishing Year : 1389

Abstract :

Structural originating of the Southern Birjand Ophiolite Mélange is required to be an implementation of various stress phases in evolutionary history of this region. Separation of different phases in the multiple inverse method shows that the maximum stress axis(σ1) in several position of this zone mainly has NE-SW to E-W trends and the minimum stress axis(σ3) NW-SE to N-S trends.

Subject List : , Stress