Propagation and termination of a strike slip fault in an extensional domain: The westward growth of the North Anatolian Fault into the Aegean Sea

Geometry and kinematics of the active submarine faults over the North Aegean Trough, a complex and highly deforming boundary zone between the Eurasian and the Anatolian/Aegean micro-plates, were examined to investigate how a strike slip motion propagates through an extensional domain. The bathymetri...
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Autor*in:	Ferentinos, George [verfasserIn] Georgiou, Nikos [verfasserIn] Christodoulou, Dimitris [verfasserIn] Geraga, Maria [verfasserIn] Papatheodorou, George [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2018

Schlagwörter:	North Anatolian Fault North Aegean Trough North Aegean extension - North Anatolian Fault interaction Strike slip - normal fault displacement transfer

Übergeordnetes Werk:	Enthalten in: Tectonophysics - Amsterdam [u.a.] : Elsevier, 1964, 745, Seite 183-195
Übergeordnetes Werk:	volume:745 ; pages:183-195

DOI / URN:	10.1016/j.tecto.2018.08.003

Katalog-ID:	ELV000909963

Internformat


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100	1		\|a Ferentinos, George \|e verfasserin \|4 aut
245	1	0	\|a Propagation and termination of a strike slip fault in an extensional domain: The westward growth of the North Anatolian Fault into the Aegean Sea
264		1	\|c 2018
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520			\|a Geometry and kinematics of the active submarine faults over the North Aegean Trough, a complex and highly deforming boundary zone between the Eurasian and the Anatolian/Aegean micro-plates, were examined to investigate how a strike slip motion propagates through an extensional domain. The bathymetric and seismic reflection data analysis show, that the investigated area is affected from east to west, by three sets of active faults striking ENE-WSW, NE-SW and WNW-ESE. The ENE-WSW and NE-SW striking faults are right lateral strike slip faults and are considered strands of the northern branch of the North Anatolian Fault into the north Aegean Sea. The former set bounds the Saros basin and the latter set occupies the eastern and central part of the Sporades Basin in the eastern and western parts of the North Aegean Trough, respectively. The WNW-ESE striking faults are normal low angle faults and develop at the western parts of the Sporades Basin. It is suggested that the strike-slip fault system advances westwards and when it reaches the 23.8°E meridian, its right lateral motion is transferred to the WNW-ESE normal faults system, forming a 70 km wide normal faulting zone through which the shear is distributed. The interaction between the strike slip and normal faults probably started with the arrival of the northern branch of the North Anatolian Fault into the western part of the Sporades Basin since 430 ka BP (Marine Isotopic Stage, 12). The described fault architecture and their spatial distribution in the North Aegean Trough are consistent with: (i) the earthquake fault plane solutions and (ii) the stress and strain pattern prevailing across the area. Furthermore, all these three provide evidence that the northern branch of the North Anatolian Fault terminates at the western end of the NAT and does not continue to central Greece.
650		4	\|a North Anatolian Fault
650		4	\|a North Aegean Trough
650		4	\|a North Aegean extension - North Anatolian Fault interaction
650		4	\|a Strike slip - normal fault displacement transfer
700	1		\|a Georgiou, Nikos \|e verfasserin \|4 aut
700	1		\|a Christodoulou, Dimitris \|e verfasserin \|4 aut
700	1		\|a Geraga, Maria \|e verfasserin \|4 aut
700	1		\|a Papatheodorou, George \|e verfasserin \|4 aut
773	0	8	\|i Enthalten in \|t Tectonophysics \|d Amsterdam [u.a.] : Elsevier, 1964 \|g 745, Seite 183-195 \|h Online-Ressource \|w (DE-627)320505952 \|w (DE-600)2012830-7 \|w (DE-576)098474197 \|x 1879-3266 \|7 nnns
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936	b	k	\|a 38.36 \|j Tektonik
936	b	k	\|a 38.58 \|j Geomechanik
951			\|a AR
952			\|d 745 \|h 183-195

Indexfelder

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publishDate	2018
allfields	10.1016/j.tecto.2018.08.003 doi (DE-627)ELV000909963 (ELSEVIER)S0040-1951(18)30282-8 DE-627 ger DE-627 rda eng 550 DE-600 38.36 bkl 38.58 bkl Ferentinos, George verfasserin aut Propagation and termination of a strike slip fault in an extensional domain: The westward growth of the North Anatolian Fault into the Aegean Sea 2018 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Geometry and kinematics of the active submarine faults over the North Aegean Trough, a complex and highly deforming boundary zone between the Eurasian and the Anatolian/Aegean micro-plates, were examined to investigate how a strike slip motion propagates through an extensional domain. The bathymetric and seismic reflection data analysis show, that the investigated area is affected from east to west, by three sets of active faults striking ENE-WSW, NE-SW and WNW-ESE. The ENE-WSW and NE-SW striking faults are right lateral strike slip faults and are considered strands of the northern branch of the North Anatolian Fault into the north Aegean Sea. The former set bounds the Saros basin and the latter set occupies the eastern and central part of the Sporades Basin in the eastern and western parts of the North Aegean Trough, respectively. The WNW-ESE striking faults are normal low angle faults and develop at the western parts of the Sporades Basin. It is suggested that the strike-slip fault system advances westwards and when it reaches the 23.8°E meridian, its right lateral motion is transferred to the WNW-ESE normal faults system, forming a 70 km wide normal faulting zone through which the shear is distributed. The interaction between the strike slip and normal faults probably started with the arrival of the northern branch of the North Anatolian Fault into the western part of the Sporades Basin since 430 ka BP (Marine Isotopic Stage, 12). The described fault architecture and their spatial distribution in the North Aegean Trough are consistent with: (i) the earthquake fault plane solutions and (ii) the stress and strain pattern prevailing across the area. Furthermore, all these three provide evidence that the northern branch of the North Anatolian Fault terminates at the western end of the NAT and does not continue to central Greece. North Anatolian Fault North Aegean Trough North Aegean extension - North Anatolian Fault interaction Strike slip - normal fault displacement transfer Georgiou, Nikos verfasserin aut Christodoulou, Dimitris verfasserin aut Geraga, Maria verfasserin aut Papatheodorou, George verfasserin aut Enthalten in Tectonophysics Amsterdam [u.a.] : Elsevier, 1964 745, Seite 183-195 Online-Ressource (DE-627)320505952 (DE-600)2012830-7 (DE-576)098474197 1879-3266 nnns volume:745 pages:183-195 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.36 Tektonik 38.58 Geomechanik AR 745 183-195
spelling	10.1016/j.tecto.2018.08.003 doi (DE-627)ELV000909963 (ELSEVIER)S0040-1951(18)30282-8 DE-627 ger DE-627 rda eng 550 DE-600 38.36 bkl 38.58 bkl Ferentinos, George verfasserin aut Propagation and termination of a strike slip fault in an extensional domain: The westward growth of the North Anatolian Fault into the Aegean Sea 2018 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Geometry and kinematics of the active submarine faults over the North Aegean Trough, a complex and highly deforming boundary zone between the Eurasian and the Anatolian/Aegean micro-plates, were examined to investigate how a strike slip motion propagates through an extensional domain. The bathymetric and seismic reflection data analysis show, that the investigated area is affected from east to west, by three sets of active faults striking ENE-WSW, NE-SW and WNW-ESE. The ENE-WSW and NE-SW striking faults are right lateral strike slip faults and are considered strands of the northern branch of the North Anatolian Fault into the north Aegean Sea. The former set bounds the Saros basin and the latter set occupies the eastern and central part of the Sporades Basin in the eastern and western parts of the North Aegean Trough, respectively. The WNW-ESE striking faults are normal low angle faults and develop at the western parts of the Sporades Basin. It is suggested that the strike-slip fault system advances westwards and when it reaches the 23.8°E meridian, its right lateral motion is transferred to the WNW-ESE normal faults system, forming a 70 km wide normal faulting zone through which the shear is distributed. The interaction between the strike slip and normal faults probably started with the arrival of the northern branch of the North Anatolian Fault into the western part of the Sporades Basin since 430 ka BP (Marine Isotopic Stage, 12). The described fault architecture and their spatial distribution in the North Aegean Trough are consistent with: (i) the earthquake fault plane solutions and (ii) the stress and strain pattern prevailing across the area. Furthermore, all these three provide evidence that the northern branch of the North Anatolian Fault terminates at the western end of the NAT and does not continue to central Greece. North Anatolian Fault North Aegean Trough North Aegean extension - North Anatolian Fault interaction Strike slip - normal fault displacement transfer Georgiou, Nikos verfasserin aut Christodoulou, Dimitris verfasserin aut Geraga, Maria verfasserin aut Papatheodorou, George verfasserin aut Enthalten in Tectonophysics Amsterdam [u.a.] : Elsevier, 1964 745, Seite 183-195 Online-Ressource (DE-627)320505952 (DE-600)2012830-7 (DE-576)098474197 1879-3266 nnns volume:745 pages:183-195 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.36 Tektonik 38.58 Geomechanik AR 745 183-195
allfields_unstemmed	10.1016/j.tecto.2018.08.003 doi (DE-627)ELV000909963 (ELSEVIER)S0040-1951(18)30282-8 DE-627 ger DE-627 rda eng 550 DE-600 38.36 bkl 38.58 bkl Ferentinos, George verfasserin aut Propagation and termination of a strike slip fault in an extensional domain: The westward growth of the North Anatolian Fault into the Aegean Sea 2018 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Geometry and kinematics of the active submarine faults over the North Aegean Trough, a complex and highly deforming boundary zone between the Eurasian and the Anatolian/Aegean micro-plates, were examined to investigate how a strike slip motion propagates through an extensional domain. The bathymetric and seismic reflection data analysis show, that the investigated area is affected from east to west, by three sets of active faults striking ENE-WSW, NE-SW and WNW-ESE. The ENE-WSW and NE-SW striking faults are right lateral strike slip faults and are considered strands of the northern branch of the North Anatolian Fault into the north Aegean Sea. The former set bounds the Saros basin and the latter set occupies the eastern and central part of the Sporades Basin in the eastern and western parts of the North Aegean Trough, respectively. The WNW-ESE striking faults are normal low angle faults and develop at the western parts of the Sporades Basin. It is suggested that the strike-slip fault system advances westwards and when it reaches the 23.8°E meridian, its right lateral motion is transferred to the WNW-ESE normal faults system, forming a 70 km wide normal faulting zone through which the shear is distributed. The interaction between the strike slip and normal faults probably started with the arrival of the northern branch of the North Anatolian Fault into the western part of the Sporades Basin since 430 ka BP (Marine Isotopic Stage, 12). The described fault architecture and their spatial distribution in the North Aegean Trough are consistent with: (i) the earthquake fault plane solutions and (ii) the stress and strain pattern prevailing across the area. Furthermore, all these three provide evidence that the northern branch of the North Anatolian Fault terminates at the western end of the NAT and does not continue to central Greece. North Anatolian Fault North Aegean Trough North Aegean extension - North Anatolian Fault interaction Strike slip - normal fault displacement transfer Georgiou, Nikos verfasserin aut Christodoulou, Dimitris verfasserin aut Geraga, Maria verfasserin aut Papatheodorou, George verfasserin aut Enthalten in Tectonophysics Amsterdam [u.a.] : Elsevier, 1964 745, Seite 183-195 Online-Ressource (DE-627)320505952 (DE-600)2012830-7 (DE-576)098474197 1879-3266 nnns volume:745 pages:183-195 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.36 Tektonik 38.58 Geomechanik AR 745 183-195
allfieldsGer	10.1016/j.tecto.2018.08.003 doi (DE-627)ELV000909963 (ELSEVIER)S0040-1951(18)30282-8 DE-627 ger DE-627 rda eng 550 DE-600 38.36 bkl 38.58 bkl Ferentinos, George verfasserin aut Propagation and termination of a strike slip fault in an extensional domain: The westward growth of the North Anatolian Fault into the Aegean Sea 2018 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Geometry and kinematics of the active submarine faults over the North Aegean Trough, a complex and highly deforming boundary zone between the Eurasian and the Anatolian/Aegean micro-plates, were examined to investigate how a strike slip motion propagates through an extensional domain. The bathymetric and seismic reflection data analysis show, that the investigated area is affected from east to west, by three sets of active faults striking ENE-WSW, NE-SW and WNW-ESE. The ENE-WSW and NE-SW striking faults are right lateral strike slip faults and are considered strands of the northern branch of the North Anatolian Fault into the north Aegean Sea. The former set bounds the Saros basin and the latter set occupies the eastern and central part of the Sporades Basin in the eastern and western parts of the North Aegean Trough, respectively. The WNW-ESE striking faults are normal low angle faults and develop at the western parts of the Sporades Basin. It is suggested that the strike-slip fault system advances westwards and when it reaches the 23.8°E meridian, its right lateral motion is transferred to the WNW-ESE normal faults system, forming a 70 km wide normal faulting zone through which the shear is distributed. The interaction between the strike slip and normal faults probably started with the arrival of the northern branch of the North Anatolian Fault into the western part of the Sporades Basin since 430 ka BP (Marine Isotopic Stage, 12). The described fault architecture and their spatial distribution in the North Aegean Trough are consistent with: (i) the earthquake fault plane solutions and (ii) the stress and strain pattern prevailing across the area. Furthermore, all these three provide evidence that the northern branch of the North Anatolian Fault terminates at the western end of the NAT and does not continue to central Greece. North Anatolian Fault North Aegean Trough North Aegean extension - North Anatolian Fault interaction Strike slip - normal fault displacement transfer Georgiou, Nikos verfasserin aut Christodoulou, Dimitris verfasserin aut Geraga, Maria verfasserin aut Papatheodorou, George verfasserin aut Enthalten in Tectonophysics Amsterdam [u.a.] : Elsevier, 1964 745, Seite 183-195 Online-Ressource (DE-627)320505952 (DE-600)2012830-7 (DE-576)098474197 1879-3266 nnns volume:745 pages:183-195 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.36 Tektonik 38.58 Geomechanik AR 745 183-195
allfieldsSound	10.1016/j.tecto.2018.08.003 doi (DE-627)ELV000909963 (ELSEVIER)S0040-1951(18)30282-8 DE-627 ger DE-627 rda eng 550 DE-600 38.36 bkl 38.58 bkl Ferentinos, George verfasserin aut Propagation and termination of a strike slip fault in an extensional domain: The westward growth of the North Anatolian Fault into the Aegean Sea 2018 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Geometry and kinematics of the active submarine faults over the North Aegean Trough, a complex and highly deforming boundary zone between the Eurasian and the Anatolian/Aegean micro-plates, were examined to investigate how a strike slip motion propagates through an extensional domain. The bathymetric and seismic reflection data analysis show, that the investigated area is affected from east to west, by three sets of active faults striking ENE-WSW, NE-SW and WNW-ESE. The ENE-WSW and NE-SW striking faults are right lateral strike slip faults and are considered strands of the northern branch of the North Anatolian Fault into the north Aegean Sea. The former set bounds the Saros basin and the latter set occupies the eastern and central part of the Sporades Basin in the eastern and western parts of the North Aegean Trough, respectively. The WNW-ESE striking faults are normal low angle faults and develop at the western parts of the Sporades Basin. It is suggested that the strike-slip fault system advances westwards and when it reaches the 23.8°E meridian, its right lateral motion is transferred to the WNW-ESE normal faults system, forming a 70 km wide normal faulting zone through which the shear is distributed. The interaction between the strike slip and normal faults probably started with the arrival of the northern branch of the North Anatolian Fault into the western part of the Sporades Basin since 430 ka BP (Marine Isotopic Stage, 12). The described fault architecture and their spatial distribution in the North Aegean Trough are consistent with: (i) the earthquake fault plane solutions and (ii) the stress and strain pattern prevailing across the area. Furthermore, all these three provide evidence that the northern branch of the North Anatolian Fault terminates at the western end of the NAT and does not continue to central Greece. North Anatolian Fault North Aegean Trough North Aegean extension - North Anatolian Fault interaction Strike slip - normal fault displacement transfer Georgiou, Nikos verfasserin aut Christodoulou, Dimitris verfasserin aut Geraga, Maria verfasserin aut Papatheodorou, George verfasserin aut Enthalten in Tectonophysics Amsterdam [u.a.] : Elsevier, 1964 745, Seite 183-195 Online-Ressource (DE-627)320505952 (DE-600)2012830-7 (DE-576)098474197 1879-3266 nnns volume:745 pages:183-195 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.36 Tektonik 38.58 Geomechanik AR 745 183-195
language	English
source	Enthalten in Tectonophysics 745, Seite 183-195 volume:745 pages:183-195
sourceStr	Enthalten in Tectonophysics 745, Seite 183-195 volume:745 pages:183-195
format_phy_str_mv	Article
bklname	Tektonik Geomechanik
institution	findex.gbv.de
topic_facet	North Anatolian Fault North Aegean Trough North Aegean extension - North Anatolian Fault interaction Strike slip - normal fault displacement transfer
dewey-raw	550
isfreeaccess_bool	false
container_title	Tectonophysics
authorswithroles_txt_mv	Ferentinos, George @@aut@@ Georgiou, Nikos @@aut@@ Christodoulou, Dimitris @@aut@@ Geraga, Maria @@aut@@ Papatheodorou, George @@aut@@
publishDateDaySort_date	2018-01-01T00:00:00Z
hierarchy_top_id	320505952
dewey-sort	3550
id	ELV000909963
language_de	englisch
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author	Ferentinos, George
spellingShingle	Ferentinos, George ddc 550 bkl 38.36 bkl 38.58 misc North Anatolian Fault misc North Aegean Trough misc North Aegean extension - North Anatolian Fault interaction misc Strike slip - normal fault displacement transfer Propagation and termination of a strike slip fault in an extensional domain: The westward growth of the North Anatolian Fault into the Aegean Sea
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topic_title	550 DE-600 38.36 bkl 38.58 bkl Propagation and termination of a strike slip fault in an extensional domain: The westward growth of the North Anatolian Fault into the Aegean Sea North Anatolian Fault North Aegean Trough North Aegean extension - North Anatolian Fault interaction Strike slip - normal fault displacement transfer
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title	Propagation and termination of a strike slip fault in an extensional domain: The westward growth of the North Anatolian Fault into the Aegean Sea
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title_full	Propagation and termination of a strike slip fault in an extensional domain: The westward growth of the North Anatolian Fault into the Aegean Sea
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author_browse	Ferentinos, George Georgiou, Nikos Christodoulou, Dimitris Geraga, Maria Papatheodorou, George
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title_sort	propagation and termination of a strike slip fault in an extensional domain: the westward growth of the north anatolian fault into the aegean sea
title_auth	Propagation and termination of a strike slip fault in an extensional domain: The westward growth of the North Anatolian Fault into the Aegean Sea
abstract	Geometry and kinematics of the active submarine faults over the North Aegean Trough, a complex and highly deforming boundary zone between the Eurasian and the Anatolian/Aegean micro-plates, were examined to investigate how a strike slip motion propagates through an extensional domain. The bathymetric and seismic reflection data analysis show, that the investigated area is affected from east to west, by three sets of active faults striking ENE-WSW, NE-SW and WNW-ESE. The ENE-WSW and NE-SW striking faults are right lateral strike slip faults and are considered strands of the northern branch of the North Anatolian Fault into the north Aegean Sea. The former set bounds the Saros basin and the latter set occupies the eastern and central part of the Sporades Basin in the eastern and western parts of the North Aegean Trough, respectively. The WNW-ESE striking faults are normal low angle faults and develop at the western parts of the Sporades Basin. It is suggested that the strike-slip fault system advances westwards and when it reaches the 23.8°E meridian, its right lateral motion is transferred to the WNW-ESE normal faults system, forming a 70 km wide normal faulting zone through which the shear is distributed. The interaction between the strike slip and normal faults probably started with the arrival of the northern branch of the North Anatolian Fault into the western part of the Sporades Basin since 430 ka BP (Marine Isotopic Stage, 12). The described fault architecture and their spatial distribution in the North Aegean Trough are consistent with: (i) the earthquake fault plane solutions and (ii) the stress and strain pattern prevailing across the area. Furthermore, all these three provide evidence that the northern branch of the North Anatolian Fault terminates at the western end of the NAT and does not continue to central Greece.
abstractGer	Geometry and kinematics of the active submarine faults over the North Aegean Trough, a complex and highly deforming boundary zone between the Eurasian and the Anatolian/Aegean micro-plates, were examined to investigate how a strike slip motion propagates through an extensional domain. The bathymetric and seismic reflection data analysis show, that the investigated area is affected from east to west, by three sets of active faults striking ENE-WSW, NE-SW and WNW-ESE. The ENE-WSW and NE-SW striking faults are right lateral strike slip faults and are considered strands of the northern branch of the North Anatolian Fault into the north Aegean Sea. The former set bounds the Saros basin and the latter set occupies the eastern and central part of the Sporades Basin in the eastern and western parts of the North Aegean Trough, respectively. The WNW-ESE striking faults are normal low angle faults and develop at the western parts of the Sporades Basin. It is suggested that the strike-slip fault system advances westwards and when it reaches the 23.8°E meridian, its right lateral motion is transferred to the WNW-ESE normal faults system, forming a 70 km wide normal faulting zone through which the shear is distributed. The interaction between the strike slip and normal faults probably started with the arrival of the northern branch of the North Anatolian Fault into the western part of the Sporades Basin since 430 ka BP (Marine Isotopic Stage, 12). The described fault architecture and their spatial distribution in the North Aegean Trough are consistent with: (i) the earthquake fault plane solutions and (ii) the stress and strain pattern prevailing across the area. Furthermore, all these three provide evidence that the northern branch of the North Anatolian Fault terminates at the western end of the NAT and does not continue to central Greece.
abstract_unstemmed	Geometry and kinematics of the active submarine faults over the North Aegean Trough, a complex and highly deforming boundary zone between the Eurasian and the Anatolian/Aegean micro-plates, were examined to investigate how a strike slip motion propagates through an extensional domain. The bathymetric and seismic reflection data analysis show, that the investigated area is affected from east to west, by three sets of active faults striking ENE-WSW, NE-SW and WNW-ESE. The ENE-WSW and NE-SW striking faults are right lateral strike slip faults and are considered strands of the northern branch of the North Anatolian Fault into the north Aegean Sea. The former set bounds the Saros basin and the latter set occupies the eastern and central part of the Sporades Basin in the eastern and western parts of the North Aegean Trough, respectively. The WNW-ESE striking faults are normal low angle faults and develop at the western parts of the Sporades Basin. It is suggested that the strike-slip fault system advances westwards and when it reaches the 23.8°E meridian, its right lateral motion is transferred to the WNW-ESE normal faults system, forming a 70 km wide normal faulting zone through which the shear is distributed. The interaction between the strike slip and normal faults probably started with the arrival of the northern branch of the North Anatolian Fault into the western part of the Sporades Basin since 430 ka BP (Marine Isotopic Stage, 12). The described fault architecture and their spatial distribution in the North Aegean Trough are consistent with: (i) the earthquake fault plane solutions and (ii) the stress and strain pattern prevailing across the area. Furthermore, all these three provide evidence that the northern branch of the North Anatolian Fault terminates at the western end of the NAT and does not continue to central Greece.
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title_short	Propagation and termination of a strike slip fault in an extensional domain: The westward growth of the North Anatolian Fault into the Aegean Sea
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author2	Georgiou, Nikos Christodoulou, Dimitris Geraga, Maria Papatheodorou, George
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doi_str	10.1016/j.tecto.2018.08.003
up_date	2024-07-06T19:35:32.329Z
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The bathymetric and seismic reflection data analysis show, that the investigated area is affected from east to west, by three sets of active faults striking ENE-WSW, NE-SW and WNW-ESE. The ENE-WSW and NE-SW striking faults are right lateral strike slip faults and are considered strands of the northern branch of the North Anatolian Fault into the north Aegean Sea. The former set bounds the Saros basin and the latter set occupies the eastern and central part of the Sporades Basin in the eastern and western parts of the North Aegean Trough, respectively. The WNW-ESE striking faults are normal low angle faults and develop at the western parts of the Sporades Basin. It is suggested that the strike-slip fault system advances westwards and when it reaches the 23.8°E meridian, its right lateral motion is transferred to the WNW-ESE normal faults system, forming a 70 km wide normal faulting zone through which the shear is distributed. The interaction between the strike slip and normal faults probably started with the arrival of the northern branch of the North Anatolian Fault into the western part of the Sporades Basin since 430 ka BP (Marine Isotopic Stage, 12). The described fault architecture and their spatial distribution in the North Aegean Trough are consistent with: (i) the earthquake fault plane solutions and (ii) the stress and strain pattern prevailing across the area. Furthermore, all these three provide evidence that the northern branch of the North Anatolian Fault terminates at the western end of the NAT and does not continue to central Greece.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">North Anatolian Fault</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">North Aegean Trough</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">North Aegean extension - North Anatolian Fault interaction</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Strike slip - normal fault displacement transfer</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Georgiou, Nikos</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Christodoulou, Dimitris</subfield><subfield code="e">verfasserin</subfield><subfield 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Propagation and termination of a strike slip fault in an extensional domain: The westward growth of the North Anatolian Fault into the Aegean Sea

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