Morphotectonics of the Padul-Nigüelas Fault Zone, southern Spain

The Padul-Nigüelas Fault Zone (PNFZ) is situated at the south-western mountain front of the Sierra Nevada (southern Spain) in the Internal Zone of the Betic Cordilleras and belongs to a NW-SE trending system of normal faults dipping SW. The PNFZ constitutes a major tectonic and lithological boundary...

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Main Authors: Jochen Hürtgen, Andreas Rudersdorf, Christoph Grützner, Klaus Reicherter
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 2014-02-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/6208
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author Jochen Hürtgen
Andreas Rudersdorf
Christoph Grützner
Klaus Reicherter
author_facet Jochen Hürtgen
Andreas Rudersdorf
Christoph Grützner
Klaus Reicherter
author_sort Jochen Hürtgen
collection DOAJ
description The Padul-Nigüelas Fault Zone (PNFZ) is situated at the south-western mountain front of the Sierra Nevada (southern Spain) in the Internal Zone of the Betic Cordilleras and belongs to a NW-SE trending system of normal faults dipping SW. The PNFZ constitutes a major tectonic and lithological boundary in the Betics, and separates the metamorphic units of the Alpujárride Complex from Upper Tertiary to Quaternary deposits. Due to recent seismicity and several morphological and geological indicators, such as preserved fault scarps, triangular facets, deeply incised valleys and faults in the colluvial wedges, the PNFZ is suspected to be a tectonically active feature of the south-eastern Granada Basin. We performed morphotectonic GIS analyses based on digital elevation models (DEM, cell size: 10 m) to obtain tectonic activity classes for each outcropping segment of the PNFZ. We have determined the following geomorphic indices: mountain front sinuosity, stream-length gradient index, concavity index and valley floor width to height ratio. The results show a differentiation in the states of activity along the fault zone strike. The western and eastern segments of the PNFZ indicate a higher tectonic activity compared to the center of the fault zone. We discuss and critically examine the comparability and reproducibility of geomorphic analyses, concluding that careful interpretation is necessary, if no ground-truthing can be performed.
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spelling doaj.art-4782c9dade2843339af755f8ef80ef0d2022-12-21T17:30:36ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X2014-02-0156610.4401/ag-62085922Morphotectonics of the Padul-Nigüelas Fault Zone, southern SpainJochen Hürtgen0Andreas Rudersdorf1Christoph Grützner2Klaus Reicherter3RWTH Aachen University, Neotectonics and Natural Hazards, Aachen,RWTH Aachen University, Neotectonics and Natural Hazards, Aachen,RWTH Aachen University, Neotectonics and Natural Hazards, Aachen,RWTH Aachen University, Neotectonics and Natural Hazards, Aachen,The Padul-Nigüelas Fault Zone (PNFZ) is situated at the south-western mountain front of the Sierra Nevada (southern Spain) in the Internal Zone of the Betic Cordilleras and belongs to a NW-SE trending system of normal faults dipping SW. The PNFZ constitutes a major tectonic and lithological boundary in the Betics, and separates the metamorphic units of the Alpujárride Complex from Upper Tertiary to Quaternary deposits. Due to recent seismicity and several morphological and geological indicators, such as preserved fault scarps, triangular facets, deeply incised valleys and faults in the colluvial wedges, the PNFZ is suspected to be a tectonically active feature of the south-eastern Granada Basin. We performed morphotectonic GIS analyses based on digital elevation models (DEM, cell size: 10 m) to obtain tectonic activity classes for each outcropping segment of the PNFZ. We have determined the following geomorphic indices: mountain front sinuosity, stream-length gradient index, concavity index and valley floor width to height ratio. The results show a differentiation in the states of activity along the fault zone strike. The western and eastern segments of the PNFZ indicate a higher tectonic activity compared to the center of the fault zone. We discuss and critically examine the comparability and reproducibility of geomorphic analyses, concluding that careful interpretation is necessary, if no ground-truthing can be performed.http://www.annalsofgeophysics.eu/index.php/annals/article/view/6208Padul-Nigüelas-Fault ZoneFault activityMorphotectonicsGeomorphic indexGranada Basin
spellingShingle Jochen Hürtgen
Andreas Rudersdorf
Christoph Grützner
Klaus Reicherter
Morphotectonics of the Padul-Nigüelas Fault Zone, southern Spain
Annals of Geophysics
Padul-Nigüelas-Fault Zone
Fault activity
Morphotectonics
Geomorphic index
Granada Basin
title Morphotectonics of the Padul-Nigüelas Fault Zone, southern Spain
title_full Morphotectonics of the Padul-Nigüelas Fault Zone, southern Spain
title_fullStr Morphotectonics of the Padul-Nigüelas Fault Zone, southern Spain
title_full_unstemmed Morphotectonics of the Padul-Nigüelas Fault Zone, southern Spain
title_short Morphotectonics of the Padul-Nigüelas Fault Zone, southern Spain
title_sort morphotectonics of the padul niguelas fault zone southern spain
topic Padul-Nigüelas-Fault Zone
Fault activity
Morphotectonics
Geomorphic index
Granada Basin
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/6208
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