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Information Journal Paper

Title

GEOMORPHIC ASSESSMENT OF ACTIVE TECTONIC IN THE SAEEDABAD-CHAI DRAINAGE BAISN (NORTH SLOPE OF SA HAND MOUNTAIN)

Pages

  67-82

Abstract

 In this study, the quaternary deformation and TECTONIC ACTIVITY of SAEEDABAD-CHAI DRAINAGE BASIN, are assessed using geomorphic approach. This drainage basin is located in northern slope of SAHAND MOUNTAIN. North Tabriz Fault (NTF), is passing from the Saeedabad-chai basin.Variation in the morphology of mountain front provides the basis for geomorphic assessment of TECTONIC ACTIVITY. Therefore, it is used from GEOMORPHIC INDEX as Stream Length Gradiant Index (SL), Asymmetry Factor (AF), Topographic Symmetry Factor (T), Drainage Basin ShapeRatio (Bs ), Mountain Front Sinusity (Smf), Ratio of valley - floor with to vally height (Vf), Percentage undissected mountain factors (Eu), Topographical maps, Digital Elevatiom Model (DEM), satellite images and Autocad map, Arc/view software. The results of this study that estimated by Index of relative active tectonic (Iat), indicated that the value of TECTONIC ACTIVITY in the SAEEDABAD-CHAI DRAINAGE BASIN, is high.

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    APA: Copy

    KARAMI, FARIBA. (2009). GEOMORPHIC ASSESSMENT OF ACTIVE TECTONIC IN THE SAEEDABAD-CHAI DRAINAGE BAISN (NORTH SLOPE OF SA HAND MOUNTAIN). PHYSICAL GEOGRAPHY RESEARCH QUARTERLY, -(69), 67-82. SID. https://sid.ir/paper/138726/en

    Vancouver: Copy

    KARAMI FARIBA. GEOMORPHIC ASSESSMENT OF ACTIVE TECTONIC IN THE SAEEDABAD-CHAI DRAINAGE BAISN (NORTH SLOPE OF SA HAND MOUNTAIN). PHYSICAL GEOGRAPHY RESEARCH QUARTERLY[Internet]. 2009;-(69):67-82. Available from: https://sid.ir/paper/138726/en

    IEEE: Copy

    FARIBA KARAMI, “GEOMORPHIC ASSESSMENT OF ACTIVE TECTONIC IN THE SAEEDABAD-CHAI DRAINAGE BAISN (NORTH SLOPE OF SA HAND MOUNTAIN),” PHYSICAL GEOGRAPHY RESEARCH QUARTERLY, vol. -, no. 69, pp. 67–82, 2009, [Online]. Available: https://sid.ir/paper/138726/en

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