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Title

Development of growth s trata in the Nesa anticline evidence on the effect of Eo-cimmerian orogeny in Central Alborz

Pages

  1-12

Abstract

 The NesaAnticline located in the southern part of the central Alborz is bounded bytheTaleghan Fault to the North andby theMoshaFault to the South. Unlike the wes tern and eas tern part of the Alborz range, in Central Alborz, the Evidence of Eo-cimmerianEventhas shown as extensional event. In this s tudy, evidence on development of Growth s trata in the NesaAnticline which can be considered as a s tructural evidneceon the performance of the Eo-cimmerianEvent in Central Alborz is presented. Inves tigations ofcross sectional mappingacross the NesaAnticline indicate a decrease in the thickness of the Triassic ElikaFormation in the anticline hinge area due to development of Growth s trata. Thisrepresentsynchronous deposition of the Elika Formation and growthof the anticline. This simultaneousfolding and sedimentation is analysed to the effect of the Eo-cimmerianEventin the s tudy area andtheCentral Alborz.

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    APA: Copy

    Zandilak, Hashem, YASSAGHI, ALI, & Madanipour, Saeed. (2018). Development of growth s trata in the Nesa anticline evidence on the effect of Eo-cimmerian orogeny in Central Alborz. TECTONICS, 2(7 ), 1-12. SID. https://sid.ir/paper/388291/en

    Vancouver: Copy

    Zandilak Hashem, YASSAGHI ALI, Madanipour Saeed. Development of growth s trata in the Nesa anticline evidence on the effect of Eo-cimmerian orogeny in Central Alborz. TECTONICS[Internet]. 2018;2(7 ):1-12. Available from: https://sid.ir/paper/388291/en

    IEEE: Copy

    Hashem Zandilak, ALI YASSAGHI, and Saeed Madanipour, “Development of growth s trata in the Nesa anticline evidence on the effect of Eo-cimmerian orogeny in Central Alborz,” TECTONICS, vol. 2, no. 7 , pp. 1–12, 2018, [Online]. Available: https://sid.ir/paper/388291/en

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