Neotectonic Activity Using Geomorphological Features in the Iraqi Kurdistan Region
Autor: | Varoujan K. Sissakian, Nadhir Al-Ansari, Lanja H. Abdullah |
---|---|
Jazyk: | angličtina |
Rok vydání: | 2020 |
Předmět: |
010504 meteorology & atmospheric sciences
Lineament Neotectonic Soil Science Pleistocene faults Active fault Deformation (meteorology) Wind gap Geotechnical Engineering 010502 geochemistry & geophysics 01 natural sciences Water gap Dissected alluvial fan Paleontology Architecture Foreland basin 0105 earth and related environmental sciences Terrane geography Hydrogeology geography.geographical_feature_category Alluvial fan Geology Geotechnical Engineering and Engineering Geology Tectonics Geoteknik |
Popis: | Iraqi Kurdistan Region is located in the northeastern part of the Arabian Plate which is colliding with the Eurasian (Iranian) Plate and is located within the Zagros Foreland Basin. This collision, which is still active with convergent type of tectonic boundary, has caused deformation of the rocks in the Zagros Foreland Basin with different intensities. The deformation intensity decreases southwest wards since the exerted stresses from the collision is in a NE–SW direction. Depending on the deformation intensity and many other factors, the tectonic framework of the region which is part of the main tectonic frame of Iraq is divided into three main tectonic units among them only two units are within Kurdistan Region. The two zones are from NE–SW direction: (1) Shalair Terrane, and (2) Outer Platform. In the current study, evidences about Neotectonic activities are presented from different parts of Kurdistan Region depending on different geomorphological and structural features. Among those features are: abnormal trends of valleys, dislocated and dissected alluvial fans, regional lineaments, water and wind gaps, faulted rocks of Pliocene–Pleistocene age, active faults. The Neotectonic evidences were recognized using satellite images and the existing Neotectonic data, and validated in the field. |
Databáze: | OpenAIRE |
Externí odkaz: |