List of Articles Geomorphic Indices

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  1 - Determination of the relative tectonics activity rate for Inehvarzan-Dalichai anticline by using geomorphic indices
  سمیه GHorbani Ahmad Alavi
  The asymmetric ENE WNW trending Inehvarzan - Dalichai anticline that is located in the East of -Damavand city and on the East of Central Alborz. This anticline consists of late Precambrian -Paleozoic - Mesozoic sediments. North limb of this anticline is confined to the More

  The asymmetric ENE WNW trending Inehvarzan - Dalichai anticline that is located in the East of -Damavand city and on the East of Central Alborz. This anticline consists of late Precambrian -Paleozoic - Mesozoic sediments. North limb of this anticline is confined to the Dehnar Mosha fault -and southern branch of this fault. South limb anticline is limited to the several secondary faults.Morphotectonic investigations including geomorphic indexes, e.g. Smf, Facet%, Af, Vf, fordetermination of the relative tectonics activity class of this anticline are carried out. The analysis ofthese indices demonstrates that North limb anticline is more active than the South limb. Manuscript profile
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  2 - The Relative Evaluation of Active Neotectonic Activities in the Kateh Pifak Anticline; Eyvan-e Qarb, Ilam
  Reza Mansouri Samad Fotoohi
  The geomorphic analysis of mountain fronts, anticlines and folded belts can provide valuable insights about the recorded tectonic history of any given region. Therefore, such studies at a regional scale have been frequently undertaken using morphotectonic analysis to de More

  The geomorphic analysis of mountain fronts, anticlines and folded belts can provide valuable insights about the recorded tectonic history of any given region. Therefore, such studies at a regional scale have been frequently undertaken using morphotectonic analysis to delineate areas having higher tectonic activity. Keteh Pifak anticline is located in the northeast of Eyvan-e-Qarb township, north of Ilam province and is considered as a part of the Zagros simply folded belt. In this research, with the aim of evaluating the active neotectonic movements in the Keteh Pifak anticline, the six geomorphic indices such as: Ratio of Valley Floor Width to Valley Height (VF), Percentage Undissected Escarpments (EU), Percentage Dissected Mountain Fronts (FD), Fold Front Sinuosity (FFS), Fold Symmetry Index (FSI), Aspect Ratio (AR) and Relative Tectonic Activity Index (Iat) have been used. The morphometry of Keteh Pifak anticline were determined using topographic maps, satellite imageries and field works. Also, the structural, tectonically and lithologically data were obtained using geological map (5257 sheets No) with 1:100,000 scale. Results show that high values of FFS, EU, AR indices and low values of FD, VF, FSI indices indicate the young and asymmetry of this anticline, the continuation of neotectonic forces and low erosion in the anticline. Also, based on the Iat index, it was determined that this anticline at class 3 of activity. Field evidence in the study area such as narrow valleys (V-shaped), straight, steep and faulted escarpments, asymmetric fold show that this anticline is tectonically relative active. Manuscript profile