TECTONIC ELEMENTS OF SOUTH FLANK IN THE EAST - CENTRAL ALBORZ MOUNTAIN

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ARIAN M.; POURKERMANI M.

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Paper Information

Journal: JOURNAL OF SCIENCE (KHARAZMI UNIVERSITY) Year:2004 | Volume:4 | Issue:1-2 Page(s): 359-368

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Title

TECTONIC ELEMENTS OF SOUTH FLANK IN THE EAST - CENTRAL ALBORZ MOUNTAIN

Author(s)

ARIAN M. | POURKERMANI M. | Issue Writer Certificate

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Abstract

Southern flank of the East- Central Alborz Mountain is consisting of several tectonic elements, which were introduced and analyzed, in this paper. This region is including a complex thrust system at north and a widespread foreland basin at south of Alborz- Central Iran border zone. Two significance curvatures at Alborz Mountain belt that have introduced here such as Neyshabur – Esfarayen - Shahrud Syntaxis and Damghan – Semnan - Qazvin Salient, had been created by change in trend of Alborz from NW- SE to NE-SW. According to this research, creative and activities of the fault systems in a sinistral displacement shear zone that had been elongated from south Semnan to north Gonbad-e Kavus was suggested as a cause to forming of above curvatures and thinning of Alborz width at north Bastam. Therefore, deformation in this region is a combination of compressional and left-lateral strike slip components that (Transpression) demonstrated by field evidences and focal mechanism solutions.

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APA: Copy

ARIAN, M., & POURKERMANI, M.. (2004). TECTONIC ELEMENTS OF SOUTH FLANK IN THE EAST - CENTRAL ALBORZ MOUNTAIN. JOURNAL OF SCIENCE (KHARAZMI UNIVERSITY), 4(1-2), 359-368. SID. https://sid.ir/paper/44010/en

Vancouver: Copy

ARIAN M., POURKERMANI M.. TECTONIC ELEMENTS OF SOUTH FLANK IN THE EAST - CENTRAL ALBORZ MOUNTAIN. JOURNAL OF SCIENCE (KHARAZMI UNIVERSITY)[Internet]. 2004;4(1-2):359-368. Available from: https://sid.ir/paper/44010/en

IEEE: Copy

M. ARIAN, and M. POURKERMANI, “TECTONIC ELEMENTS OF SOUTH FLANK IN THE EAST - CENTRAL ALBORZ MOUNTAIN,” JOURNAL OF SCIENCE (KHARAZMI UNIVERSITY), vol. 4, no. 1-2, pp. 359–368, 2004, [Online]. Available: https://sid.ir/paper/44010/en

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