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Information Journal Paper

Title

MICROSTRUCTURE ANALYSIS OF ZARAB REGION, SOUTH OF KERMAN

Pages

  259-270

Abstract

 Zarab region situated in south of Baft city and Northern Boundary of Sanandaj-Sirjan zone. Petrographical studies indicate Rock units get moderately green schist facies metamorphism grade and contain of: orthogenesis, Marble and abundance schist's in Zarab region.We can see flow structures in marble and various MICROSTRUCTURES as like S-C structures, and structures Mica Fishes and et… in schist' s. We could recognize dextral shear sense, which caused MICROSTRUCTURES. The amounts of tension strains in normal section that prepared from oriented samples indicate prolate form strain ellipsoid parallel to schistosity fabrics. Field studies show, which the thrust faults, have a dextral movement (co orientation with MICROSTRUCTURES shear sense), similar orientation, slip movement and absence of fault plan erosion. Varieties between faulting deformation (brittle deformation) and shear sense of MICROSTRUCTURES (ductile deformation), reveal two deformation phase with a nonconcurring deformation time and brittle deformation took place in second stage.

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  • Cite

    APA: Copy

    IRANMANESH, F., SHAFIEI BAFTI, A., SHAHRIARI, S., & POURKERMANI, M.. (2009). MICROSTRUCTURE ANALYSIS OF ZARAB REGION, SOUTH OF KERMAN. JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY), 4(4), 259-270. SID. https://sid.ir/paper/127103/en

    Vancouver: Copy

    IRANMANESH F., SHAFIEI BAFTI A., SHAHRIARI S., POURKERMANI M.. MICROSTRUCTURE ANALYSIS OF ZARAB REGION, SOUTH OF KERMAN. JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY)[Internet]. 2009;4(4):259-270. Available from: https://sid.ir/paper/127103/en

    IEEE: Copy

    F. IRANMANESH, A. SHAFIEI BAFTI, S. SHAHRIARI, and M. POURKERMANI, “MICROSTRUCTURE ANALYSIS OF ZARAB REGION, SOUTH OF KERMAN,” JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY), vol. 4, no. 4, pp. 259–270, 2009, [Online]. Available: https://sid.ir/paper/127103/en

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