Evaluation of the Relative Tectonic Activity of the Adıyaman fault within the Arabian-Anatolian plate boundary (eastern Turkey)

The left-lateral strike-slip Adıyaman fault is located in eastern Turkey within the plate boundary deformation zone between Arabia and Anatolia. The Adıyaman fault is a major splay from the East Anatolian Fault (EAF), one of the most important tectonic structures in the Eastern Mediterranean region....

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Main Authors: A. Khalifa, Z. Çakir, L.A. Owen, Ş. Kaya
Format: Article
Language:English
Published: Universitat de Barcelona (UB), Geociències Barcelona (Geo3BCN), Institut de Diagnosi Ambiental i Estudis de l'Aigua (IDAEA), Universitat Autònoma de Barcelona (UAB) 2019-06-01
Series:Geologica Acta
Subjects:
Online Access:https://revistes.ub.edu/index.php/GEOACTA/article/view/GeologicaActa2019.17.6/29352
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author A. Khalifa
Z. Çakir
L.A. Owen
Ş. Kaya
author_facet A. Khalifa
Z. Çakir
L.A. Owen
Ş. Kaya
author_sort A. Khalifa
collection DOAJ
description The left-lateral strike-slip Adıyaman fault is located in eastern Turkey within the plate boundary deformation zone between Arabia and Anatolia. The Adıyaman fault is a major splay from the East Anatolian Fault (EAF), one of the most important tectonic structures in the Eastern Mediterranean region. These faults are consequence of the collision between the Arabian and Anatolian plates and the resulting westward tectonic escape of Anatolia. Although the EAF has been intensively studied since its discovery in the late 1960s, little is known about the Adıyaman fault and its tectonic activity. In this study, we extract geomorphic indices including mountain-front sinuosity (Smf), valley floor width-to-height ratio (Vf), stream length-gradient (SL), catchment Asymmetry Factor (AF) and hypsometric integrals and curves (HI and HC) to evaluate the relative tectonic activity of the Adıyaman fault. These three geomorphic indices (AF, HI, and HC) are averaged to define an index for Relative Tectonic Activity (RTA) that allows the Adıyaman fault to be divided into categories of low, moderate and high RTA. The results confirm that the Adıyaman fault is an active fault with high to moderate Quaternary tectonic activity. However, this fault is of minor importance on accommodating plate boundary deformation, as evidenced by the recent crustal motions determined by GPS studies. Nevertheless, it is worthwhile to note that the Adıyaman fault still poses a significant seismic hazard for the region despite its relatively moderate tectonic activity.
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spelling doaj.art-647ea453324143a18d26aecab1583c162023-10-18T11:00:57ZengUniversitat de Barcelona (UB), Geociències Barcelona (Geo3BCN), Institut de Diagnosi Ambiental i Estudis de l'Aigua (IDAEA), Universitat Autònoma de Barcelona (UAB)Geologica Acta1696-57282019-06-0117611710.1344/GeologicaActa2019.17.6Evaluation of the Relative Tectonic Activity of the Adıyaman fault within the Arabian-Anatolian plate boundary (eastern Turkey)A. Khalifa0Z. Çakir1L.A. Owen2Ş. Kaya3Department of Geological Engineering, Faculty of Mines, Istanbul Technical UniversityDepartment of Geological Engineering, Faculty of Mines, Istanbul Technical UniversityDepartment of Geology, University of CincinnatiDepartment of Geomatics, Faculty of Civil Engineering, Istanbul Technical UniversityThe left-lateral strike-slip Adıyaman fault is located in eastern Turkey within the plate boundary deformation zone between Arabia and Anatolia. The Adıyaman fault is a major splay from the East Anatolian Fault (EAF), one of the most important tectonic structures in the Eastern Mediterranean region. These faults are consequence of the collision between the Arabian and Anatolian plates and the resulting westward tectonic escape of Anatolia. Although the EAF has been intensively studied since its discovery in the late 1960s, little is known about the Adıyaman fault and its tectonic activity. In this study, we extract geomorphic indices including mountain-front sinuosity (Smf), valley floor width-to-height ratio (Vf), stream length-gradient (SL), catchment Asymmetry Factor (AF) and hypsometric integrals and curves (HI and HC) to evaluate the relative tectonic activity of the Adıyaman fault. These three geomorphic indices (AF, HI, and HC) are averaged to define an index for Relative Tectonic Activity (RTA) that allows the Adıyaman fault to be divided into categories of low, moderate and high RTA. The results confirm that the Adıyaman fault is an active fault with high to moderate Quaternary tectonic activity. However, this fault is of minor importance on accommodating plate boundary deformation, as evidenced by the recent crustal motions determined by GPS studies. Nevertheless, it is worthwhile to note that the Adıyaman fault still poses a significant seismic hazard for the region despite its relatively moderate tectonic activity.https://revistes.ub.edu/index.php/GEOACTA/article/view/GeologicaActa2019.17.6/29352tectonic geomorphologygeomorphic indicesadıyaman strike-slip faulteastern turkey
spellingShingle A. Khalifa
Z. Çakir
L.A. Owen
Ş. Kaya
Evaluation of the Relative Tectonic Activity of the Adıyaman fault within the Arabian-Anatolian plate boundary (eastern Turkey)
Geologica Acta
tectonic geomorphology
geomorphic indices
adıyaman strike-slip fault
eastern turkey
title Evaluation of the Relative Tectonic Activity of the Adıyaman fault within the Arabian-Anatolian plate boundary (eastern Turkey)
title_full Evaluation of the Relative Tectonic Activity of the Adıyaman fault within the Arabian-Anatolian plate boundary (eastern Turkey)
title_fullStr Evaluation of the Relative Tectonic Activity of the Adıyaman fault within the Arabian-Anatolian plate boundary (eastern Turkey)
title_full_unstemmed Evaluation of the Relative Tectonic Activity of the Adıyaman fault within the Arabian-Anatolian plate boundary (eastern Turkey)
title_short Evaluation of the Relative Tectonic Activity of the Adıyaman fault within the Arabian-Anatolian plate boundary (eastern Turkey)
title_sort evaluation of the relative tectonic activity of the adiyaman fault within the arabian anatolian plate boundary eastern turkey
topic tectonic geomorphology
geomorphic indices
adıyaman strike-slip fault
eastern turkey
url https://revistes.ub.edu/index.php/GEOACTA/article/view/GeologicaActa2019.17.6/29352
work_keys_str_mv AT akhalifa evaluationoftherelativetectonicactivityoftheadıyamanfaultwithinthearabiananatolianplateboundaryeasternturkey
AT zcakir evaluationoftherelativetectonicactivityoftheadıyamanfaultwithinthearabiananatolianplateboundaryeasternturkey
AT laowen evaluationoftherelativetectonicactivityoftheadıyamanfaultwithinthearabiananatolianplateboundaryeasternturkey
AT skaya evaluationoftherelativetectonicactivityoftheadıyamanfaultwithinthearabiananatolianplateboundaryeasternturkey