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Environmental Monitoring and Assessment, 2018
Coastal tsunami amplitudes were calculated to identify areas susceptible to tsunami hazard at selected locations of the coast of Karnataka, west of India, due to earthquakes in the Makran Subduction Zone. This is the first time that the probabilistic tsunami hazard assessment along this study area has been attempted.
Sowmya, K +2 more
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Coastal tsunami amplitudes were calculated to identify areas susceptible to tsunami hazard at selected locations of the coast of Karnataka, west of India, due to earthquakes in the Makran Subduction Zone. This is the first time that the probabilistic tsunami hazard assessment along this study area has been attempted.
Sowmya, K +2 more
openaire +2 more sources
Investigation of seismic stress changes in Makran subduction zone
2022Mostafazadeh, Mehrdad, Mahshadnia, Leila
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Seismological Research Letters
Abstract Large, distant earthquakes can trigger deep tectonic tremors in subduction zones and other seismically active regions. Although most documented cases occur along the Pacific Rim, only a few have been identified in the Alpine-Himalayan orogenic belt and the Sumatra-Java subduction zones.
Jie Chen +6 more
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Abstract Large, distant earthquakes can trigger deep tectonic tremors in subduction zones and other seismically active regions. Although most documented cases occur along the Pacific Rim, only a few have been identified in the Alpine-Himalayan orogenic belt and the Sumatra-Java subduction zones.
Jie Chen +6 more
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Journal of Geophysical Research: Solid Earth
Abstract Subduction zones are key in shaping seismic hazards, yet many remain poorly understood. The Western Makran Subduction Zone (WMSZ) is a good example of a challenging hazard assessment due to its low seismic activity and limited geodetic data.
A. Sobouti +5 more
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Abstract Subduction zones are key in shaping seismic hazards, yet many remain poorly understood. The Western Makran Subduction Zone (WMSZ) is a good example of a challenging hazard assessment due to its low seismic activity and limited geodetic data.
A. Sobouti +5 more
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Seismic waveforms from CIGSIP project seismic array in the western Makran subduction zone
The Waveform_bag zip package includes waveform events for 5 mainshocks (seismic information in Table 1) recorded on 39 stations up to 2 hours after the beginning of the earthquake. Each station has five components: Z, N, E, R, and T. The instrumental response was not removed from each record, and the instrumental response file see the PZ_file.dat.openaire +1 more source
A landslide tsunami hazard assessment in the Makran Subduction Zone
Marine GeologyAmin Rashidi +4 more
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