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(a) The horizontal component of the acceleration time history (Acc) recorde...
Published: 01 October 2012
Figure 8. (a) The horizontal component of the acceleration time history (Acc) recorded at the ORIO and ORHO stations (from the earthquake of 24 December 2008). (b) Comparison between the simulated and recorded acceleration time history for the ORHO station. (c) The soil amplification curve based
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Val-des-Bois  M  3.0 earthquake on 31 December 2008, recorded by the ORHO s...
Published: 01 December 2011
Figure 7. Val-des-Bois M  3.0 earthquake on 31 December 2008, recorded by the ORHO station (soil) and the nearby ORIO station (rock). The solid line shows the spectral ratio of the ORHO station (soil) to the ORIO station (rock), and the dashed line shows the spectral ratio of the horizontal
Image
Sample seismic stations (a) A11, (b) A64, (c) GAC, and (d) <span class="search-highlight">ORIO</span>, mean horiz...
Published: 15 August 2023
Figure 5. Sample seismic stations (a) A11, (b) A64, (c) GAC, and (d) ORIO, mean horizontal‐to‐vertical spectral ratio (HVSR) from earthquake records (black dashed) and microtremor data (dotted gray; Ladak, 2020 ; Ladak et al. 2021 ), and amplification functions (solid color lines
Journal Article
Journal: AAPG Bulletin
Published: 01 November 1978
AAPG Bulletin (1978) 62 (11): 2232–2242.
... of 5° for the coastal region between Deva and Fuenterrabia which includes the area studied here. Such a plunge would be negligible. The Late Cretaceous and early Tertiary flysch deposits in the area between San Sebastian and Orio tilt north-northwest with a strike of about 70° but the beds near...
FIGURES | View All (8)
Series: Geological Society, London, Special Publications
Published: 23 August 2023
DOI: 10.1144/SP528-2022-70
EISBN: 9781786209603
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ChirpProfile (trasf_0; modified from  I <span class="search-highlight">orio</span>  e t  a lii , 2014b ) showing ...
Published: 01 June 2017
Fig. 4 ChirpProfile (trasf_0; modified from I orio e t a lii , 2014b ) showing the seismo-stratigraphic architecture of the area (see location in Fig. 1 ). Notice the volcanic marker (V) marked in red. See text for explanation.
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Chirp Profiles M198A (modified from  I <span class="search-highlight">orio</span>  e t  a lii , 2014b ), M199 and...
Published: 01 June 2017
Fig. 6 Chirp Profiles M198A (modified from I orio e t a lii , 2014b ), M199 and M200 (see location in Fig. 1 ). Notice the volcanic marker (V) marked in red. See text for the explanation.
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PSA ratio between the soil site (ORHO) and the reference bedrock station (O...
Published: 01 October 2012
Figure 5. PSA ratio between the soil site (ORHO) and the reference bedrock station (ORIO) for two representative earthquakes.
Journal Article
Published: 01 October 2012
Bulletin of the Seismological Society of America (2012) 102 (5): 1976–1993.
...Figure 8. (a) The horizontal component of the acceleration time history (Acc) recorded at the ORIO and ORHO stations (from the earthquake of 24 December 2008). (b) Comparison between the simulated and recorded acceleration time history for the ORHO station. (c) The soil amplification curve based...
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—Model showing tectonic deformations of Eocene layers between <span class="search-highlight">Orio</span> and Zara...
Published: 01 November 1978
Fig. 5 —Model showing tectonic deformations of Eocene layers between Orio and Zarauz with reconstruction of strike lines and current directions. Sheet corresponds to “second sandstone unit” which crops out along dotted line on map.
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Residuals (after adjustments for  Q  and geometrical spreading) for the hor...
Published: 15 August 2023
Figure 11. Residuals (after adjustments for Q and geometrical spreading) for the horizontal component at 20.1 Hz for stations (a) A16, (b) ORIO, (c) OTT, and (d) A64, respectively. The black symbols show mean binned distance residual (black circle) with standard deviation bars (black whiskers).
Journal Article
Published: 01 June 2017
Italian Journal of Geosciences (2017) 136 (2): 263–274.
...Fig. 4 ChirpProfile (trasf_0; modified from I orio e t a lii , 2014b ) showing the seismo-stratigraphic architecture of the area (see location in Fig. 1 ). Notice the volcanic marker (V) marked in red. See text for explanation. ...
FIGURES | View All (8)
Journal Article
Published: 17 May 2024
Journal of the Geological Society (2024) 181 (4): jgs2023-173.
FIGURES | View All (10)
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A comparison of the  SV  waves for the Ladysmith mainshock and some of the ...
Published: 28 January 2015
Figure 14. A comparison of the SV waves for the Ladysmith mainshock and some of the aftershocks at station ORIO (distance 70–75 km). The number beside each trace refers to its order of occurrence within the sequence; additional details are in Table  2 .
Journal Article
Published: 01 December 2011
Bulletin of the Seismological Society of America (2011) 101 (6): 2942–2954.
...Figure 7. Val-des-Bois M  3.0 earthquake on 31 December 2008, recorded by the ORHO station (soil) and the nearby ORIO station (rock). The solid line shows the spectral ratio of the ORHO station (soil) to the ORIO station (rock), and the dashed line shows the spectral ratio of the horizontal...
FIGURES | View All (13)
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(I) Grain size, (II) Lithology and (III) Raw Volume Magnetic susceptibility...
Published: 01 June 2017
Fig. 2 (I) Grain size, (II) Lithology and (III) Raw Volume Magnetic susceptibility logs of core C1161. Black star and label V indicate the stratigraphic height of tephra sample and the top of the volcanic marker, respectively (modified from I orio e t a lii , 2014b ).
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The time-series recording of the Val-des-Bois  M  3.0 earthquake on 31 Dece...
Published: 01 December 2011
Figure 6. The time-series recording of the Val-des-Bois M  3.0 earthquake on 31 December 2008 at an epicentral distance of 77 km from ORHO (gray lines) and ORIO (black lines) stations. (a) East–west components, (b) north–south components, and (c) vertical components.
Journal Article
Published: 14 June 2023
Journal of the Geological Society (2023) 180 (4): jgs2022-143.
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Journal Article
Published: 01 July 2021
American Mineralogist (2021) 106 (7): 1172–1182.
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Journal Article
Published: 07 March 2017
Journal of the Geological Society (2017) 174 (4): 609–626.
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