Tectonic geomorphology of the Şemdinli Yüksekova fault zone (SYFZ) and Başkale fault zone (BFZ) (SE Turkey)

The collision between the Arabian and Eurasian plates resulted in the uplift of The East Anatolian Province of Shortening (EAPS). Within the EAPS, the faulting mechanism is characterized by right- and left-lateral strike-slip faults, thrust faults, and a relatively limited occurrence of normal fault...

Descripción completa

Detalles Bibliográficos
Autor: Mutlu, Sacit|||0000-0003-1632-722X
Tipo de recurso: artículo
Fecha de publicación:2025
País:España
Institución:Universitat Autònoma de Barcelona
Repositorio:Dipòsit Digital de Documents de la UAB
Idioma:inglés
OAI Identifier:oai:ddd.uab.cat:322512
Acceso en línea:https://ddd.uab.cat/record/322512
https://dx.doi.org/urn:doi:10.1344/GeologicaActa2025.23.23
Access Level:acceso abierto
Palabra clave:Başkale fault
Deformation sharing
Morphometric index
Tectonic geomorphology
Şemdinli-yüksekova fault
id ES_b79dfd5afb0f100e671c89ff14c6c2c5
oai_identifier_str oai:ddd.uab.cat:322512
network_acronym_str ES
network_name_str España
repository_id_str
spelling Tectonic geomorphology of the Şemdinli Yüksekova fault zone (SYFZ) and Başkale fault zone (BFZ) (SE Turkey)evidence from morphometric analysis and neotectonic structuresMutlu, Sacit|||0000-0003-1632-722XBaşkale faultDeformation sharingMorphometric indexTectonic geomorphologyŞemdinli-yüksekova faultThe collision between the Arabian and Eurasian plates resulted in the uplift of The East Anatolian Province of Shortening (EAPS). Within the EAPS, the faulting mechanism is characterized by right- and left-lateral strike-slip faults, thrust faults, and a relatively limited occurrence of normal faults. When examined on a regional tectonic scale, about 70% of the deformation of the EAPS is controlled by strike-slip faults. However, the proportion of right- and left-lateral strike-slip faults contributing to this deformation remains unknown and is poorly understood. Two adjacent fault zones located at the southeastern margin of EAPS were selected to investigate the deformation associated with right- and left-lateral strike-slip mechanisms using morphometric analysis along with field observations. These fault zones are the Şemdinli Yüksekova Fault Zone (ŞYFZ), which exhibits right lateral deformation and is defined as a seismic gap, and the Başkale Fault Zone (BFZ), which has a left lateral deformation and that caused a destructive earthquake in (23/02/2020 ,Mw:5.9). To elucidate the relative degree of active tectonics of both fault zones, morphometric analysis were applied alongside field surveys. An adaptation of the Relative active tectonic index (Iat) was computed for Başkale and Yüksekova-Şemdinli sub-basins in the region. The results supported by field observations indicate that the drainage basins are largely controlled by fault activity and exhibit a youthful topographic character. Moreover, quantitative data derived from the Index of Active Tectonics (IAT) reveal that the Şemdinli-Yüksekova Fault Zone (SYFZ) demonstrates very high tectonic activity, while the Başkale Fault Zone (BFZ) displays moderate levels of active tectonic deformation. These numerical findings, which indicate ongoing deformation, are further corroborated by field observations that clearly reflect the surface expressions of tectonic activity. 22025-01-0120252025-01-01Articlehttp://purl.org/coar/resource_type/c_6501VoRhttp://purl.org/coar/version/c_970fb48d4fbd8a85info:eu-repo/semantics/articleapplication/pdfhttps://ddd.uab.cat/record/322512https://dx.doi.org/urn:doi:10.1344/GeologicaActa2025.23.23reponame:Dipòsit Digital de Documents de la UABinstname:Universitat Autònoma de BarcelonaInglésengopen accesshttp://purl.org/coar/access_right/c_abf2Aquest document està subjecte a una llicència d'ús Creative Commons. Es permet la reproducció total o parcial, la distribució, la comunicació pública de l'obra i la creació d'obres derivades, sempre i quan aquestes es distribueixin sota la mateixa llicència que regula l'obra original i es reconegui l'autoria.https://creativecommons.org/licenses/by-sa/4.0/info:eu-repo/semantics/openAccessoai:ddd.uab.cat:3225122026-06-06T12:50:31Z
dc.title.none.fl_str_mv Tectonic geomorphology of the Şemdinli Yüksekova fault zone (SYFZ) and Başkale fault zone (BFZ) (SE Turkey)
evidence from morphometric analysis and neotectonic structures
title Tectonic geomorphology of the Şemdinli Yüksekova fault zone (SYFZ) and Başkale fault zone (BFZ) (SE Turkey)
spellingShingle Tectonic geomorphology of the Şemdinli Yüksekova fault zone (SYFZ) and Başkale fault zone (BFZ) (SE Turkey)
Mutlu, Sacit|||0000-0003-1632-722X
Başkale fault
Deformation sharing
Morphometric index
Tectonic geomorphology
Şemdinli-yüksekova fault
title_short Tectonic geomorphology of the Şemdinli Yüksekova fault zone (SYFZ) and Başkale fault zone (BFZ) (SE Turkey)
title_full Tectonic geomorphology of the Şemdinli Yüksekova fault zone (SYFZ) and Başkale fault zone (BFZ) (SE Turkey)
title_fullStr Tectonic geomorphology of the Şemdinli Yüksekova fault zone (SYFZ) and Başkale fault zone (BFZ) (SE Turkey)
title_full_unstemmed Tectonic geomorphology of the Şemdinli Yüksekova fault zone (SYFZ) and Başkale fault zone (BFZ) (SE Turkey)
title_sort Tectonic geomorphology of the Şemdinli Yüksekova fault zone (SYFZ) and Başkale fault zone (BFZ) (SE Turkey)
dc.creator.none.fl_str_mv Mutlu, Sacit|||0000-0003-1632-722X
author Mutlu, Sacit|||0000-0003-1632-722X
author_facet Mutlu, Sacit|||0000-0003-1632-722X
author_role author
dc.subject.none.fl_str_mv Başkale fault
Deformation sharing
Morphometric index
Tectonic geomorphology
Şemdinli-yüksekova fault
topic Başkale fault
Deformation sharing
Morphometric index
Tectonic geomorphology
Şemdinli-yüksekova fault
description The collision between the Arabian and Eurasian plates resulted in the uplift of The East Anatolian Province of Shortening (EAPS). Within the EAPS, the faulting mechanism is characterized by right- and left-lateral strike-slip faults, thrust faults, and a relatively limited occurrence of normal faults. When examined on a regional tectonic scale, about 70% of the deformation of the EAPS is controlled by strike-slip faults. However, the proportion of right- and left-lateral strike-slip faults contributing to this deformation remains unknown and is poorly understood. Two adjacent fault zones located at the southeastern margin of EAPS were selected to investigate the deformation associated with right- and left-lateral strike-slip mechanisms using morphometric analysis along with field observations. These fault zones are the Şemdinli Yüksekova Fault Zone (ŞYFZ), which exhibits right lateral deformation and is defined as a seismic gap, and the Başkale Fault Zone (BFZ), which has a left lateral deformation and that caused a destructive earthquake in (23/02/2020 ,Mw:5.9). To elucidate the relative degree of active tectonics of both fault zones, morphometric analysis were applied alongside field surveys. An adaptation of the Relative active tectonic index (Iat) was computed for Başkale and Yüksekova-Şemdinli sub-basins in the region. The results supported by field observations indicate that the drainage basins are largely controlled by fault activity and exhibit a youthful topographic character. Moreover, quantitative data derived from the Index of Active Tectonics (IAT) reveal that the Şemdinli-Yüksekova Fault Zone (SYFZ) demonstrates very high tectonic activity, while the Başkale Fault Zone (BFZ) displays moderate levels of active tectonic deformation. These numerical findings, which indicate ongoing deformation, are further corroborated by field observations that clearly reflect the surface expressions of tectonic activity.
publishDate 2025
dc.date.none.fl_str_mv 2
2025-01-01
2025
2025-01-01
dc.type.none.fl_str_mv Article
http://purl.org/coar/resource_type/c_6501
VoR
http://purl.org/coar/version/c_970fb48d4fbd8a85
dc.type.openaire.fl_str_mv info:eu-repo/semantics/article
format article
dc.identifier.none.fl_str_mv https://ddd.uab.cat/record/322512
https://dx.doi.org/urn:doi:10.1344/GeologicaActa2025.23.23
url https://ddd.uab.cat/record/322512
https://dx.doi.org/urn:doi:10.1344/GeologicaActa2025.23.23
dc.language.none.fl_str_mv Inglés
eng
language_invalid_str_mv Inglés
language eng
dc.rights.none.fl_str_mv open access
http://purl.org/coar/access_right/c_abf2
https://creativecommons.org/licenses/by-sa/4.0/
dc.rights.openaire.fl_str_mv info:eu-repo/semantics/openAccess
rights_invalid_str_mv open access
http://purl.org/coar/access_right/c_abf2
https://creativecommons.org/licenses/by-sa/4.0/
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.source.none.fl_str_mv reponame:Dipòsit Digital de Documents de la UAB
instname:Universitat Autònoma de Barcelona
instname_str Universitat Autònoma de Barcelona
reponame_str Dipòsit Digital de Documents de la UAB
collection Dipòsit Digital de Documents de la UAB
repository.name.fl_str_mv
repository.mail.fl_str_mv
_version_ 1869417543550107648
score 15,811543