The Lâalam (Béjaïa, North-East Algeria) Moderate Earthquake ($ M_{w} $ = 5.2) on March 20, 2006
Abstract On March 20, 2006, a moderate-magnitude earthquake of $ M_{w} $ 5.2 hit the region of the Babors mountains, a region located two hundred km east of Algiers (capital of Algeria). More precisely, the epicentre occurred 40 km south-east of Béjaïa, the second most important city in the Kabylian...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Beldjoudi, H. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2009 |
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| Schlagwörter: |
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| Anmerkung: |
© Birkhäuser Verlag, Basel 2009 |
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| Übergeordnetes Werk: |
Enthalten in: Pure and applied geophysics - Birkhäuser-Verlag, 1964, 166(2009), 4 vom: Apr., Seite 623-640 |
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| Übergeordnetes Werk: |
volume:166 ; year:2009 ; number:4 ; month:04 ; pages:623-640 |
| Links: |
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| DOI / URN: |
10.1007/s00024-009-0462-9 |
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| Katalog-ID: |
OLC2069491110 |
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| 245 | 1 | 0 | |a The Lâalam (Béjaïa, North-East Algeria) Moderate Earthquake ($ M_{w} $ = 5.2) on March 20, 2006 |
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| 520 | |a Abstract On March 20, 2006, a moderate-magnitude earthquake of $ M_{w} $ 5.2 hit the region of the Babors mountains, a region located two hundred km east of Algiers (capital of Algeria). More precisely, the epicentre occurred 40 km south-east of Béjaïa, the second most important city in the Kabylian region. The earthquake impacted an area with a radius of about 70 km and caused the death of four persons and injured 68. Damage was mainly observed in Lâalam village (district of Kherrata) where some buildings and old houses were affected. Damage was mainly due to a moderate landslide triggered by the earthquake. Rock falls were also observed near the main cliffs. The maximum observed intensity $ I_{0} $ was estimated to VII (EMS-98 scale). According to the main shock focal mechanism solution and the spatial distribution of aftershocks, the main shock was reliably found to have been generated by an NS sinistral strike-slip fault. The compressive stress axis $ σ_{1} $, oriented N325, is in agreement with the direction of convergence between Eurasia and Africa. | ||
| 650 | 4 | |a Lâalam earthquake | |
| 650 | 4 | |a Lâalam landslide | |
| 650 | 4 | |a Stress tensor inversion | |
| 650 | 4 | |a Aftershock study | |
| 650 | 4 | |a Babors chain seismicity | |
| 700 | 1 | |a Guemache, M. A. |4 aut | |
| 700 | 1 | |a Kherroubi, A. |4 aut | |
| 700 | 1 | |a Semmane, F. |4 aut | |
| 700 | 1 | |a Yelles-Chaouche, A. K. |4 aut | |
| 700 | 1 | |a Djellit, H. |4 aut | |
| 700 | 1 | |a Amrani, A. |4 aut | |
| 700 | 1 | |a Haned, A. |4 aut | |
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10.1007/s00024-009-0462-9 doi (DE-627)OLC2069491110 (DE-He213)s00024-009-0462-9-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Beldjoudi, H. verfasserin aut The Lâalam (Béjaïa, North-East Algeria) Moderate Earthquake ($ M_{w} $ = 5.2) on March 20, 2006 2009 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Birkhäuser Verlag, Basel 2009 Abstract On March 20, 2006, a moderate-magnitude earthquake of $ M_{w} $ 5.2 hit the region of the Babors mountains, a region located two hundred km east of Algiers (capital of Algeria). More precisely, the epicentre occurred 40 km south-east of Béjaïa, the second most important city in the Kabylian region. The earthquake impacted an area with a radius of about 70 km and caused the death of four persons and injured 68. Damage was mainly observed in Lâalam village (district of Kherrata) where some buildings and old houses were affected. Damage was mainly due to a moderate landslide triggered by the earthquake. Rock falls were also observed near the main cliffs. The maximum observed intensity $ I_{0} $ was estimated to VII (EMS-98 scale). According to the main shock focal mechanism solution and the spatial distribution of aftershocks, the main shock was reliably found to have been generated by an NS sinistral strike-slip fault. The compressive stress axis $ σ_{1} $, oriented N325, is in agreement with the direction of convergence between Eurasia and Africa. Lâalam earthquake Lâalam landslide Stress tensor inversion Aftershock study Babors chain seismicity Guemache, M. A. aut Kherroubi, A. aut Semmane, F. aut Yelles-Chaouche, A. K. aut Djellit, H. aut Amrani, A. aut Haned, A. aut Enthalten in Pure and applied geophysics Birkhäuser-Verlag, 1964 166(2009), 4 vom: Apr., Seite 623-640 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:166 year:2009 number:4 month:04 pages:623-640 https://doi.org/10.1007/s00024-009-0462-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4155 GBV_ILN_4277 AR 166 2009 4 04 623-640 |
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10.1007/s00024-009-0462-9 doi (DE-627)OLC2069491110 (DE-He213)s00024-009-0462-9-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Beldjoudi, H. verfasserin aut The Lâalam (Béjaïa, North-East Algeria) Moderate Earthquake ($ M_{w} $ = 5.2) on March 20, 2006 2009 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Birkhäuser Verlag, Basel 2009 Abstract On March 20, 2006, a moderate-magnitude earthquake of $ M_{w} $ 5.2 hit the region of the Babors mountains, a region located two hundred km east of Algiers (capital of Algeria). More precisely, the epicentre occurred 40 km south-east of Béjaïa, the second most important city in the Kabylian region. The earthquake impacted an area with a radius of about 70 km and caused the death of four persons and injured 68. Damage was mainly observed in Lâalam village (district of Kherrata) where some buildings and old houses were affected. Damage was mainly due to a moderate landslide triggered by the earthquake. Rock falls were also observed near the main cliffs. The maximum observed intensity $ I_{0} $ was estimated to VII (EMS-98 scale). According to the main shock focal mechanism solution and the spatial distribution of aftershocks, the main shock was reliably found to have been generated by an NS sinistral strike-slip fault. The compressive stress axis $ σ_{1} $, oriented N325, is in agreement with the direction of convergence between Eurasia and Africa. Lâalam earthquake Lâalam landslide Stress tensor inversion Aftershock study Babors chain seismicity Guemache, M. A. aut Kherroubi, A. aut Semmane, F. aut Yelles-Chaouche, A. K. aut Djellit, H. aut Amrani, A. aut Haned, A. aut Enthalten in Pure and applied geophysics Birkhäuser-Verlag, 1964 166(2009), 4 vom: Apr., Seite 623-640 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:166 year:2009 number:4 month:04 pages:623-640 https://doi.org/10.1007/s00024-009-0462-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4155 GBV_ILN_4277 AR 166 2009 4 04 623-640 |
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10.1007/s00024-009-0462-9 doi (DE-627)OLC2069491110 (DE-He213)s00024-009-0462-9-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Beldjoudi, H. verfasserin aut The Lâalam (Béjaïa, North-East Algeria) Moderate Earthquake ($ M_{w} $ = 5.2) on March 20, 2006 2009 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Birkhäuser Verlag, Basel 2009 Abstract On March 20, 2006, a moderate-magnitude earthquake of $ M_{w} $ 5.2 hit the region of the Babors mountains, a region located two hundred km east of Algiers (capital of Algeria). More precisely, the epicentre occurred 40 km south-east of Béjaïa, the second most important city in the Kabylian region. The earthquake impacted an area with a radius of about 70 km and caused the death of four persons and injured 68. Damage was mainly observed in Lâalam village (district of Kherrata) where some buildings and old houses were affected. Damage was mainly due to a moderate landslide triggered by the earthquake. Rock falls were also observed near the main cliffs. The maximum observed intensity $ I_{0} $ was estimated to VII (EMS-98 scale). According to the main shock focal mechanism solution and the spatial distribution of aftershocks, the main shock was reliably found to have been generated by an NS sinistral strike-slip fault. The compressive stress axis $ σ_{1} $, oriented N325, is in agreement with the direction of convergence between Eurasia and Africa. Lâalam earthquake Lâalam landslide Stress tensor inversion Aftershock study Babors chain seismicity Guemache, M. A. aut Kherroubi, A. aut Semmane, F. aut Yelles-Chaouche, A. K. aut Djellit, H. aut Amrani, A. aut Haned, A. aut Enthalten in Pure and applied geophysics Birkhäuser-Verlag, 1964 166(2009), 4 vom: Apr., Seite 623-640 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:166 year:2009 number:4 month:04 pages:623-640 https://doi.org/10.1007/s00024-009-0462-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4155 GBV_ILN_4277 AR 166 2009 4 04 623-640 |
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the lâalam (béjaïa, north-east algeria) moderate earthquake ($ m_{w} $ = 5.2) on march 20, 2006 |
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The Lâalam (Béjaïa, North-East Algeria) Moderate Earthquake ($ M_{w} $ = 5.2) on March 20, 2006 |
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Abstract On March 20, 2006, a moderate-magnitude earthquake of $ M_{w} $ 5.2 hit the region of the Babors mountains, a region located two hundred km east of Algiers (capital of Algeria). More precisely, the epicentre occurred 40 km south-east of Béjaïa, the second most important city in the Kabylian region. The earthquake impacted an area with a radius of about 70 km and caused the death of four persons and injured 68. Damage was mainly observed in Lâalam village (district of Kherrata) where some buildings and old houses were affected. Damage was mainly due to a moderate landslide triggered by the earthquake. Rock falls were also observed near the main cliffs. The maximum observed intensity $ I_{0} $ was estimated to VII (EMS-98 scale). According to the main shock focal mechanism solution and the spatial distribution of aftershocks, the main shock was reliably found to have been generated by an NS sinistral strike-slip fault. The compressive stress axis $ σ_{1} $, oriented N325, is in agreement with the direction of convergence between Eurasia and Africa. © Birkhäuser Verlag, Basel 2009 |
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Abstract On March 20, 2006, a moderate-magnitude earthquake of $ M_{w} $ 5.2 hit the region of the Babors mountains, a region located two hundred km east of Algiers (capital of Algeria). More precisely, the epicentre occurred 40 km south-east of Béjaïa, the second most important city in the Kabylian region. The earthquake impacted an area with a radius of about 70 km and caused the death of four persons and injured 68. Damage was mainly observed in Lâalam village (district of Kherrata) where some buildings and old houses were affected. Damage was mainly due to a moderate landslide triggered by the earthquake. Rock falls were also observed near the main cliffs. The maximum observed intensity $ I_{0} $ was estimated to VII (EMS-98 scale). According to the main shock focal mechanism solution and the spatial distribution of aftershocks, the main shock was reliably found to have been generated by an NS sinistral strike-slip fault. The compressive stress axis $ σ_{1} $, oriented N325, is in agreement with the direction of convergence between Eurasia and Africa. © Birkhäuser Verlag, Basel 2009 |
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Abstract On March 20, 2006, a moderate-magnitude earthquake of $ M_{w} $ 5.2 hit the region of the Babors mountains, a region located two hundred km east of Algiers (capital of Algeria). More precisely, the epicentre occurred 40 km south-east of Béjaïa, the second most important city in the Kabylian region. The earthquake impacted an area with a radius of about 70 km and caused the death of four persons and injured 68. Damage was mainly observed in Lâalam village (district of Kherrata) where some buildings and old houses were affected. Damage was mainly due to a moderate landslide triggered by the earthquake. Rock falls were also observed near the main cliffs. The maximum observed intensity $ I_{0} $ was estimated to VII (EMS-98 scale). According to the main shock focal mechanism solution and the spatial distribution of aftershocks, the main shock was reliably found to have been generated by an NS sinistral strike-slip fault. The compressive stress axis $ σ_{1} $, oriented N325, is in agreement with the direction of convergence between Eurasia and Africa. © Birkhäuser Verlag, Basel 2009 |
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