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Cites:

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Information Journal Paper

Title

ACTIVE TECTONIC IN BINALUD MOUNTAIN WITH RESPECT TO MORPHOTECTONIC

Pages

  79-91

Abstract

 Introduction: Tectonic of Binaloud mountain ranges is controled by thrust faults system and folds related to these faults. Parts of this mountain ranges and NEYSHABOUR plain is as study area in north eastern Iran and between latitudes 36o 11’ 00 to 36o 30´ 00 and longitudes 58o 35´ 00 to 59o 00´ 00. In this paper we first study morphometric indices in this area then analyze DRAINAGEs and allovial fans to identify activity of Binaloud mountain.materials and Methods: In order to identify activities in Binaloud mountain, studing morphometric indices and analysis of DRAINAGE network together be done. The first step for calculating morphometric analysis in the region is to digitize topographical maps with the scale 1:50000 by ArcGIS software to extract required data and then morphometrical data is formulized and calculated exactly and the results is interpreted.

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    APA: Copy

    SHAFIEE, E., ALAVI, A., & NADERI MIGHAN, N.. (2010). ACTIVE TECTONIC IN BINALUD MOUNTAIN WITH RESPECT TO MORPHOTECTONIC. PHYSICAL GEOGRAPHY RESEARCH QUARTERLY, -(70), 79-91. SID. https://sid.ir/paper/138865/en

    Vancouver: Copy

    SHAFIEE E., ALAVI A., NADERI MIGHAN N.. ACTIVE TECTONIC IN BINALUD MOUNTAIN WITH RESPECT TO MORPHOTECTONIC. PHYSICAL GEOGRAPHY RESEARCH QUARTERLY[Internet]. 2010;-(70):79-91. Available from: https://sid.ir/paper/138865/en

    IEEE: Copy

    E. SHAFIEE, A. ALAVI, and N. NADERI MIGHAN, “ACTIVE TECTONIC IN BINALUD MOUNTAIN WITH RESPECT TO MORPHOTECTONIC,” PHYSICAL GEOGRAPHY RESEARCH QUARTERLY, vol. -, no. 70, pp. 79–91, 2010, [Online]. Available: https://sid.ir/paper/138865/en

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