QUATERNARY DEFORMATION IN THE WEST OF SHAHROOD (EAST ALBORZ)

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AARAB F.; OMIDY P.; TAHERI A.

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Journal: GEOSCIENCES Year:2011 | Volume:20 | Issue:80 Page(s): 89-94

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Title

QUATERNARY DEFORMATION IN THE WEST OF SHAHROOD (EAST ALBORZ)

Author(s)

AARAB F. | OMIDY P. | TAHERI A. | Issue Writer Certificate

Keywords

QUATERNARY DEFORMATIONQ2

EAST ALBORZQ2

WEST OF SHAHROODQ3

DEH-MOLLAQ2

TAZAREHQ2

ASTANEH FAULTQ2

Abstract

In this paper, the evidences of QUATERNARY DEFORMATION in the WEST OF SHAHROOD, in an area starting from DEH-MOLLA valley and extending to TAZAREH valley in the southern domain of eastern Alborz have been studied. The studied area is bounded on the North and South by two main faults that trends east- west and dips to north. In the field inspection, the evidences of Quaternary activity like cutting and displacing of Quaternary sediments in some localities such as DEH-MOLLA and TAZAREH valleys have been observed. This study showed that the indications of Quaternary activity are present in the whole of the region; but the North fault with a dominantly left lateral strike slip mechanism that is the eastern continuation of ASTANEH FAULT, has a main role in QUATERNARY DEFORMATION. The left lateral strike slip movement on South fault is finished to east where it connects to a normal transfer fault. This latter transfer fault trends north- south and dips to east.

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APA: Copy

AARAB, F., OMIDY, P., & TAHERI, A.. (2011). QUATERNARY DEFORMATION IN THE WEST OF SHAHROOD (EAST ALBORZ). GEOSCIENCES, 20(80), 89-94. SID. https://sid.ir/paper/31432/en

Vancouver: Copy

AARAB F., OMIDY P., TAHERI A.. QUATERNARY DEFORMATION IN THE WEST OF SHAHROOD (EAST ALBORZ). GEOSCIENCES[Internet]. 2011;20(80):89-94. Available from: https://sid.ir/paper/31432/en

IEEE: Copy

F. AARAB, P. OMIDY, and A. TAHERI, “QUATERNARY DEFORMATION IN THE WEST OF SHAHROOD (EAST ALBORZ),” GEOSCIENCES, vol. 20, no. 80, pp. 89–94, 2011, [Online]. Available: https://sid.ir/paper/31432/en

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