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  • 04.06. Seismology  (1)
  • 05.08. Risk  (1)
  • Area/locality; Calculated; ELEVATION; Heat flow; Heat production, average; LATITUDE; LONGITUDE; Method comment; Number; Number of temperature data; Sample, optional label/labor no; Temperature gradient
  • Atlantic; Binary Object; Binary Object (File Size); Elevation of event; Event label; File content; FRAME-OBS; FRAME-OBS_OBH100; FRAME-OBS_OBH101; FRAME-OBS_OBH102; FRAME-OBS_OBH103; FRAME-OBS_OBH76; FRAME-OBS_OBH77; FRAME-OBS_OBH78; FRAME-OBS_OBH79; FRAME-OBS_OBH80; FRAME-OBS_OBH81; FRAME-OBS_OBH88; FRAME-OBS_OBH89; FRAME-OBS_OBH90; FRAME-OBS_OBH91; FRAME-OBS_OBH92; FRAME-OBS_OBH93; FRAME-OBS_OBS104; FRAME-OBS_OBS105; FRAME-OBS_OBS82; FRAME-OBS_OBS83; FRAME-OBS_OBS84; FRAME-OBS_OBS85; FRAME-OBS_OBS86; FRAME-OBS_OBS87; FRAME-OBS_OBS94; FRAME-OBS_OBS95; FRAME-OBS_OBS96; FRAME-OBS_OBS97; FRAME-OBS_OBS98; FRAME-OBS_OBS99; FRAME-OBS_P03; Latitude of event; Longitude of event; OBH; OBS; Ocean bottom hydrophone; ocean-bottom-hydrophones; ocean bottom seismometer; Ocean bottom seismometer; oceanic crust; passive continental margin; Portuguese Margin; S03; Sarmiento de Gamboa; seismic data; Seismic refraction profile; SEISREFR; South Atlantic Ocean
  • Binary Object; Binary Object (File Size); Continental rifting; continent-ocean transition; Event label; Line; OBH; OBH 02; OBH 04; OBH 06; OBH 08; OBH 26; OBH 30; OBH 32; OBH 56; OBH 58; OBH 60; OBH 62; OBH 63; OBH 65; OBH 67; OBH 68; OBH 70; OBS; OBS 11; OBS 16; OBS 17; OBS 18; OBS 19; OBS 20; OBS 22; OBS 23; OBS 24; OBS 28; OBS 34; OBS 38; OBS 40; OBS 42; OBS 43; OBS 46; OBS 48; OBS 52; OBS 54; OBS 59; OBS 64; OBS 69; OBS 7; OBS 73; OBS 75; Ocean bottom hydrophone; Ocean bottom seismometer; POS453; POS453_724-1; POS453_729-1; POS453_731-1; POS453_734-1; POS453_736-1; POS453_738-1; POS453_740-1; POS453_742-1; POS453_746-1; POS453_748-1; POS453_751-1; POS453_752-1; POS453_754-1; POS453_755-1; POS453_757-1; POS453_763-1; POS453_766-1; POS453_768-1; POS453_773-1; POS453_774-1; POS453_775-1; POS453_776-1; POS453_779-1; POS453_780-1; POS453_781-1; POS453_791-1; POS453_792-1; POS453_793-1; POS453_794-1; POS453_795-1; POS453_796-1; POS453_797-1; POS453_798-1; POS453_799-1; POS453_820-1; POS453_821-1; POS453_822-1; POS453_823-1; POS453_824-1; POS453_825-1; POS453_826-1; Poseidon; Station label; Type; West Iberia; wide-angle seismic
  • Magnetotellurics
  • Multichannel Seismic reflection
  • Elsevier  (1)
Sammlung
Schlagwörter
  • 04.06. Seismology  (1)
  • 05.08. Risk  (1)
  • Area/locality; Calculated; ELEVATION; Heat flow; Heat production, average; LATITUDE; LONGITUDE; Method comment; Number; Number of temperature data; Sample, optional label/labor no; Temperature gradient
  • Atlantic; Binary Object; Binary Object (File Size); Elevation of event; Event label; File content; FRAME-OBS; FRAME-OBS_OBH100; FRAME-OBS_OBH101; FRAME-OBS_OBH102; FRAME-OBS_OBH103; FRAME-OBS_OBH76; FRAME-OBS_OBH77; FRAME-OBS_OBH78; FRAME-OBS_OBH79; FRAME-OBS_OBH80; FRAME-OBS_OBH81; FRAME-OBS_OBH88; FRAME-OBS_OBH89; FRAME-OBS_OBH90; FRAME-OBS_OBH91; FRAME-OBS_OBH92; FRAME-OBS_OBH93; FRAME-OBS_OBS104; FRAME-OBS_OBS105; FRAME-OBS_OBS82; FRAME-OBS_OBS83; FRAME-OBS_OBS84; FRAME-OBS_OBS85; FRAME-OBS_OBS86; FRAME-OBS_OBS87; FRAME-OBS_OBS94; FRAME-OBS_OBS95; FRAME-OBS_OBS96; FRAME-OBS_OBS97; FRAME-OBS_OBS98; FRAME-OBS_OBS99; FRAME-OBS_P03; Latitude of event; Longitude of event; OBH; OBS; Ocean bottom hydrophone; ocean-bottom-hydrophones; ocean bottom seismometer; Ocean bottom seismometer; oceanic crust; passive continental margin; Portuguese Margin; S03; Sarmiento de Gamboa; seismic data; Seismic refraction profile; SEISREFR; South Atlantic Ocean
  • Binary Object; Binary Object (File Size); Continental rifting; continent-ocean transition; Event label; Line; OBH; OBH 02; OBH 04; OBH 06; OBH 08; OBH 26; OBH 30; OBH 32; OBH 56; OBH 58; OBH 60; OBH 62; OBH 63; OBH 65; OBH 67; OBH 68; OBH 70; OBS; OBS 11; OBS 16; OBS 17; OBS 18; OBS 19; OBS 20; OBS 22; OBS 23; OBS 24; OBS 28; OBS 34; OBS 38; OBS 40; OBS 42; OBS 43; OBS 46; OBS 48; OBS 52; OBS 54; OBS 59; OBS 64; OBS 69; OBS 7; OBS 73; OBS 75; Ocean bottom hydrophone; Ocean bottom seismometer; POS453; POS453_724-1; POS453_729-1; POS453_731-1; POS453_734-1; POS453_736-1; POS453_738-1; POS453_740-1; POS453_742-1; POS453_746-1; POS453_748-1; POS453_751-1; POS453_752-1; POS453_754-1; POS453_755-1; POS453_757-1; POS453_763-1; POS453_766-1; POS453_768-1; POS453_773-1; POS453_774-1; POS453_775-1; POS453_776-1; POS453_779-1; POS453_780-1; POS453_781-1; POS453_791-1; POS453_792-1; POS453_793-1; POS453_794-1; POS453_795-1; POS453_796-1; POS453_797-1; POS453_798-1; POS453_799-1; POS453_820-1; POS453_821-1; POS453_822-1; POS453_823-1; POS453_824-1; POS453_825-1; POS453_826-1; Poseidon; Station label; Type; West Iberia; wide-angle seismic
  • +
Verlag/Herausgeber
Erscheinungszeitraum
  • 1
    Publikationsdatum: 2022-02-22
    Beschreibung: The westernmost Mediterranean hosts part of the plate boundary between the European and African tectonic plates. Based on the scattered instrumental seismicity, this boundary has been traditionally interpreted as a wide zone of diffuse deformation. However, recent seismic images and seafloor mapping studies support that most of the plate convergence may be accommodated in a few tectonic structures, rather than in a broad region. Historical earthquakes with magnitudes Mw 〉 6 and historical tsunamis support that the low-to-moderate instrumental seismicity might also have led to underestimation of the seismogenic and tsunamigenic potential of the area. We evaluate the largest active faults of the westernmost Mediterranean: the reverse Alboran Ridge, and the strike-slip Carboneras, Yusuf and Al-Idrissi fault systems. For the first time, we use a dense grid of modern seismic data to characterize the entire dimensions of the main fault systems, accurately describe the geometry of these structures and estimate their seismic source parameters. Tsunami scenarios have been tested based on 3D-surfaces and seismic source parameters, using both uniform and heterogeneous slip distributions. The comparison of our results with previous studies, based on limited information on the fault geometry and kinematics, indicates that accurate fault geometries and heterogeneous slip distributions are needed to properly assess the seismic and tsunamigenic potential in this area. Based on fault scaling relations, the four fault systems have a large seismogenic potential, being able to generate earthquakes with Mw 〉 7. The reverse Alboran Ridge Fault System has the largest tsunamigenic potential, being able to generate a tsunami wave amplitude greater than 3 m in front of the coasts of Southern Spain and Northern Africa.
    Beschreibung: Published
    Beschreibung: 106749
    Beschreibung: 6T. Studi di pericolosità sismica e da maremoto
    Beschreibung: JCR Journal
    Schlagwort(e): Western Mediterranean ; Seismogenic potential ; Tsunamigenic potential ; Numerical modelling ; Active faults ; Active seismic data ; 04.04. Geology ; 04.07. Tectonophysics ; 04.06. Seismology ; 05.08. Risk
    Repository-Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Materialart: article
    Standort Signatur Erwartet Verfügbarkeit
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