The reliability estimations involve a nonlinear analysis for the dynamic responses of the structure, calculated via a step by step procedure over the complete earthquake record.
To understand the complex linear surface ruptures along the Futagawa and Hinagu fault zones as well as the complete earthquake sequence, further study using not only crustal deformation but a combination of other tools, such as seismic wave analysis, would be required.
We used a complete and homogeneous earthquake catalog (Yadav et al. 2008 in Pure and Applied Geophysics 165, 1813 1833) comprising 15 intra-continent earthquake events (M ≥ 5.0) that occurred in the Kachchh region (23 25° N, 68 71° E) during 1819 to 2006.
Based on this result, a study about the relationship between building characteristics, site condition, and the damage level based on probabilistic analysis was regarded as important to give a complete understanding of earthquake damage pattern in Yogyakarta.
A complete catalog of earthquakes with consistent magnitudes can provide necessary data for studying the distribution of earthquakes in a region as a function of space, time, and magnitude.
Our purpose has been simply to obtain the evolution pattern of ΣM0 prior to the occurrence of large earthquakes, for providing an additional tool for seismic hazard assessment, even if the duration of our current seismic record is too short compared with a complete cycle of large earthquakes.
We compare the timing of earthquakes greater than M 5 with the temporal and spatial passage of surface waves generated by large earthquakes using a complete worldwide catalogue.
Borehole breakout orientations indicate the stress state of the hanging wall is in normal fault regime and a complete stress drop occurred during the earthquake (Lin et al. 2013).
The government has identified five main goals to achieve by 2030: a clean and economical energy system, a healthy and active aging society, a framework of next generation infrastructures, substantial economic benefits through regional and international collaborations, and a complete recovery from the Great East Japan Earthquake of 2011.
We picked P- and S-wave arrival times of earthquakes to produce a complete hypocenter catalogue, carried out double-difference event relocations, and then determined focal mechanism solutions of 7 earthquakes from P-wave polarity data.
