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Information Journal Paper

Title

STRUCTURAL EVOLUTION OF ALBURZ MOUNTAIN AND ITS RELATED SEDIMENTATION

Pages

  141-162

Keywords

Not Registered.

Abstract

 A part of Alburz Mountains which is located between Damghan plain (in the south) and Gorgan plain (in the north) structurally is a S-SE vergence thin-skinned fold-thrust belt. Sequential thrusting and related folding during Cimmerian and Alpine orogeny have been the most deformation style since late Triassic. Tectonostratigraphy of Alburz Based on foreland stratigraphical evolution models reveals that structural evolution of Alburz had taken place at three stages: 1) Late Triassic - Early Jurassic duo to Cimmerides; 2) Late Cretaceous - Early Paleocene duo to middle Alpine compress ional movements; 3) Neogene duo to Late Alpine compress ional movements. South - ward migration of Alburz in each stage accompanied by generation of new thrust faults, uplift and unroofing in fold- thrust belt and caused southward marine transgression and synorogenic classic sedimentation in Foreland basin. Each stage of structural evolution followed by a relaxation period that is characterized by isostatic rebound, reducing of erosion and shallow marine sedimentation in foreland basin duo to north ward marine regression.

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  • Cite

    APA: Copy

    SHAHRIARI, S., MOUSAVI HARAMI, SEYED REZA, & RAHIMI, B.. (2002). STRUCTURAL EVOLUTION OF ALBURZ MOUNTAIN AND ITS RELATED SEDIMENTATION . JOURNAL OF SCIENCE (KHARAZMI UNIVERSITY), 1(3-4), 141-162. SID. https://sid.ir/paper/43928/en

    Vancouver: Copy

    SHAHRIARI S., MOUSAVI HARAMI SEYED REZA, RAHIMI B.. STRUCTURAL EVOLUTION OF ALBURZ MOUNTAIN AND ITS RELATED SEDIMENTATION . JOURNAL OF SCIENCE (KHARAZMI UNIVERSITY)[Internet]. 2002;1(3-4):141-162. Available from: https://sid.ir/paper/43928/en

    IEEE: Copy

    S. SHAHRIARI, SEYED REZA MOUSAVI HARAMI, and B. RAHIMI, “STRUCTURAL EVOLUTION OF ALBURZ MOUNTAIN AND ITS RELATED SEDIMENTATION ,” JOURNAL OF SCIENCE (KHARAZMI UNIVERSITY), vol. 1, no. 3-4, pp. 141–162, 2002, [Online]. Available: https://sid.ir/paper/43928/en

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