STRUCTURAL EVIDENCES OF CONTINENTAL TRANSPRESSION IN THE BIRK AREA (SE IRAN)

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MOUSAVI E.

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Journal: GEOSCIENCES Year:2011 | Volume:20 | Issue:79 Page(s): 75-82

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Title

STRUCTURAL EVIDENCES OF CONTINENTAL TRANSPRESSION IN THE BIRK AREA (SE IRAN)

Author(s)

MOUSAVI E. | Issue Writer Certificate

Keywords

TRANSPRESSIONQ2

SISTANQ2

BIRKQ2

Abstract

Some structural evidences of continental TRANSPRESSION are studied and compared with experimental modeling results in the BIRK area. These evidences are: fold axes have a double plunging en-echelon pattern. Fold axes mean orientations and fracture cleavages strike form angles less than 45 degrees with the boundary faults. Strike-slip faults have an en-echelon and domainal pattern. Synthetic P Shears are more abundant than synthetic R shears. Flat tension vein (and normal faults) planes lie at a high-angle with respect to folds axes and this condition proposes some amounts of hinge-parallel extensions. Inclined dextral layer-parallel detachment faults and related structures such as asymmetric dextrally verging minor folds, traspressional and trastensional faults and large-scale half flower structures are other structural features of dextral TRANSPRESSION. It is believed that partitioning of dextral component of wrench-dominated continental TRANSPRESSION is due to reactivation of N-S striking basement faults in late Neogene.

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APA: Copy

MOUSAVI, E.. (2011). STRUCTURAL EVIDENCES OF CONTINENTAL TRANSPRESSION IN THE BIRK AREA (SE IRAN). GEOSCIENCES, 20(79), 75-82. SID. https://sid.ir/paper/31549/en

Vancouver: Copy

MOUSAVI E.. STRUCTURAL EVIDENCES OF CONTINENTAL TRANSPRESSION IN THE BIRK AREA (SE IRAN). GEOSCIENCES[Internet]. 2011;20(79):75-82. Available from: https://sid.ir/paper/31549/en

IEEE: Copy

E. MOUSAVI, “STRUCTURAL EVIDENCES OF CONTINENTAL TRANSPRESSION IN THE BIRK AREA (SE IRAN),” GEOSCIENCES, vol. 20, no. 79, pp. 75–82, 2011, [Online]. Available: https://sid.ir/paper/31549/en

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