--> The Strike – Slip Faults Morphotectonic in The Foreland Belt –Iraq
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The Previous HitStrikeNext Hit – Slip Faults Morphotectonic in The Foreland Belt –Iraq

Alaa Hamdon1

1Geosciences school / Aberdeen university

May 18, 2015 Monday 10:20 P.M. European Regional Conference and Exhibition, Lisbon, Portugal

Abstract

This study is concerned on the morphotectonic analysis of the Previous HitstrikeNext Hit-slip faults in the Foreland belt – northern Iraq and focused on the tectonic stress that generated them. Depending on the morphotectonic features which are noticed from visual interpretation and field work of selected areas, the Previous HitstrikeNext Hit-slip faults have been recognized in this belt. These features were influence the other geological structures (e.g. folds, river, drainage Pattern and Previous HitdipNext Hit-slip fault).

The morphotectonic analysis has been carried out in this study by followings:-

  • Using Remote Sensing techniques on the satellite images to determine the location and magnitude of the Previous HitstrikeNext Hit-slip faults by visual interpretation and digital techniques.
  • Locating and demonstrating the Previous HitstrikeNext Hit-slip faults for selected areas by using remote sensing data. Then, segregate the morphotectonic changes due to the effect of these faults on the surrounded structures such as (changing of rock beds' Previous HitdipNext Hit, modifying of anticline plunge's direction, diverging of drainage pattern and deformation in alluvial fan's shape).
  • Preparing thematic maps (morphotectonic) for each Previous HitstrikeNext Hit-slip fault in the selected areas according to the (ITC) system for morphotectonic classification.
  • Stress analysis for the explored Previous HitstrikeNext Hit-slip faults in the study area by using Anderson analysis's system for conjugate faults.
  • Definition the tectonic environments that constructed by the Previous HitstrikeNext Hit-slip faults and the complex structures which are resulted from it such as (Pull-apart basin, shear zone and horsetail structure).
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    As a final result from compilation and discussion of above quantitative and qualitative results, which are extracted from remote sensing data. Comparing that result with the ground geological facts for the study area. Then, specify the morphotectonic framework of the Previous HitstrikeTop-slip faults for the Foreland belt of northern Iraq. The relation of these faults with the other geological structures clarified by constructed a specific morphotectonic map for this purpose at scale (1:300000).

    AAPG Datapages/Search and Discovery Article #90226 © 2015 European Regional Conference and Exhibition, Lisbon, Portugal, May 18-19, 2015