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Bakar-Vinodol Fault

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(a) Summary of seismic intensities for the 1750 Croatia earthquake by Herak et al. (2017). Intensities range up to VIII (Medvedev–Sponheuer–Karnik scale) according to the percentage of black filling in circles. Gray (red in the online version) and white stars indicate the new and older estimates of the epicenter. The simplified trace of the Bakar–Vinodol fault (in gray, in red in the online version, ticks on upthrown side) is after Benac et al. (2008). Rectangular box indicates the horizontal projection of the finite‐fault model derived from inversion of the amount of tectonic subsidence in marine notches in the wider Rijeka area; a continuous line indicates predicted surface faulting. Seismic uplift is expected to the northwest, seismic subsidence to the southeast of the fault (see panel b and Stiros and Moschas, 2012). (b) Projection of the depth of marine notches, formed at mean sea level during the post‐Roman period (last 2000 yrs) along an axis normal to the mean trend of the Bakar–Vinodol thrust (see panel a). Two different groups of notch depth are evident, notches with a uniform depth of 55 cm at the wider part of the Rijeka Gulf, indicative of effects associated with a global sea‐level rise, and notch depths increasing to 115 cm in the vicinity of the Bakar area, conspicuously because of tectonic activity. Observed and model‐predicted tectonic subsidence and notch depth is also shown. Based on Stiros and Moschas (2012).The color version of this figure is available only in the electronic edition.
Published: 20 September 2017
and older estimates of the epicenter. The simplified trace of the BakarVinodol fault (in gray, in red in the online version, ticks on upthrown side) is after Benac et al. (2008) . Rectangular box indicates the horizontal projection of the finite‐fault model derived from inversion of the amount
Journal Article
Published: 20 September 2017
Seismological Research Letters (2017) 88 (6): 1534–1536.
... and older estimates of the epicenter. The simplified trace of the BakarVinodol fault (in gray, in red in the online version, ticks on upthrown side) is after Benac et al. (2008) . Rectangular box indicates the horizontal projection of the finite‐fault model derived from inversion of the amount...
FIGURES
Journal Article
Published: 20 September 2017
Seismological Research Letters (2017) 88 (6): 1537–1538.
... fault (assumed to be the BakarVinodol fault system in S2017) nor addressed the enigma of tidal notches of the northern Adriatic, we shall not comment on the source model presented in S2017 (reproduced from Stiros and Moschas, 2012 ). We, however, do agree that the 1750 Bakar earthquake is the most...
Journal Article
Published: 12 April 2017
Seismological Research Letters (2017) 88 (3): 904–915.
...Davorka Herak; Ivica Sović; Ina Cecić; Mladen Živčić; Iva Dasović; Marijan Herak ABSTRACT We present macroseismic analyses of three historical earthquakes that occurred in 1750, 1838, and 1904 in the Bakar epicentral area (Rijeka region, Croatia). Using various historical sources, we were able...
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Journal Article
Published: 30 May 2018
Seismological Research Letters (2018) 89 (4): 1524–1536.
... ) that, according to Placer et al. (2010) , cuts vertically through major thrust structures (e.g., the Snežnik thrust). A similar picture is seen farther to the southeast, where the steeply dipping Klana‐Novi Vinodolski fault intersects structures of the Vinodol thrust fault zone at a shallow depth...
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