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Information Journal Paper

Title

SEPARATION OF PALEOSTRESSES PHASES WITH INVERSION METHOD OF FAULT PLANES IN THE SOUTH OF BIRJAND REGION

Pages

  27-37

Abstract

 Structural originating of the SOUTHERN BIRJAND OPHIOLITE MÉLANGE is required to be an implementation of various stress phases in the evolution history of this region. Separation of different phases in the multiple inverse method shows that the maximum stress axis (s1) in several position of this zone has mainly NE-SW to E-W trends and the minimum stress axis (s3) NW-SE to N-S trends. By using obtained stress orientations and compiling them with the other obtained structural data, such as extensional structures (normal faults and extensional fractures), compressional structures (thrust faults, lineation and foliation trends in flysch units and the orientation of folds axes), shear-comperssional structures (fracture types in the crashed zones) and extensional structures (strike-slip faults with normal tensor, extensional and sigmoidal fractures), it is concluded that paleotectonic of this region has been affected by three stages including comperssional, shear-compersional and extensional.

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  • Cite

    APA: Copy

    MOUSSAVI, M., ALAVI, A., & KHATIB, M.M.. (2010). SEPARATION OF PALEOSTRESSES PHASES WITH INVERSION METHOD OF FAULT PLANES IN THE SOUTH OF BIRJAND REGION. IRANIAN JOURNAL OF GEOLOGY, 4(13), 27-37. SID. https://sid.ir/paper/129294/en

    Vancouver: Copy

    MOUSSAVI M., ALAVI A., KHATIB M.M.. SEPARATION OF PALEOSTRESSES PHASES WITH INVERSION METHOD OF FAULT PLANES IN THE SOUTH OF BIRJAND REGION. IRANIAN JOURNAL OF GEOLOGY[Internet]. 2010;4(13):27-37. Available from: https://sid.ir/paper/129294/en

    IEEE: Copy

    M. MOUSSAVI, A. ALAVI, and M.M. KHATIB, “SEPARATION OF PALEOSTRESSES PHASES WITH INVERSION METHOD OF FAULT PLANES IN THE SOUTH OF BIRJAND REGION,” IRANIAN JOURNAL OF GEOLOGY, vol. 4, no. 13, pp. 27–37, 2010, [Online]. Available: https://sid.ir/paper/129294/en

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