The strong motion recordings of the analyzed Vrancea earthquakes as well as the MSK intensity pattern of the 1977 earthquake can be well reproduced using relatively small strong motion generation areas, which corresponds to small asperities with high stress drops (300 1200 bar) and high particle velocities (3 5 m/s).
A collection of ground motion recordings of small to moderate (3.0 3.5≤ML≤6.5) earthquakes obtained during the execution of the Taiwan Strong Motion Instrumentation Program TSMIPP) since 1991 was used to study source scaling model, attenuation relations and site effects in Taiwan region.
(b) Strong-motion recordings of the 11 March 2011, Tohoku, Japan earthquake recorded by the TAIPEI 101 building seismic array at T1S1 on the fifth floor underground, at T1S2 on the 74 th floor, at T1S3 and T1S4 on the 90th floor, and at 101B broadband down hole station.
A database of strong ground-motion recordings of 36 earthquakes, which happened in Iran's tectonic regions, is used to establish the model.
For motion recordings, the spatial positions of the marker clusters on bony segments, including thorax, scapula, and upper arm, were captured using four Optotrak (Northern Digital Inc., Canada, nominal accuracy 0.3 mm) camera bars with the sampling frequency of 50 Hz.
We have also obtained a number of strong motion recordings from India and Nepal seismic network and developed an empirical relationship between the MMI and peak ground acceleration (PGA), peak ground velocity (PGV).
The geophysical signals available to address this problem include seismic and geodetic ground motion recordings, tsunami recordings, aftershock distributions, and in some cases, bathymetric pressure sensors and imaging of coseismic changes in the seafloor.
The analysis and representation are applied to motion capture recordings of dance performances of popular dance styles and the process of validation compares different parameters applied to the representation model according to a set of evaluation criteria.
Because of the lack of strong-motion recordings at the sites of damaged buildings, it is not clear whether the damage was due to large ground motions.
Nepal and the Himalayan regions in general have not obtained the number of strong-motion recordings necessary for seismic hazard analysis because of the sparse and underdeveloped strong-motion monitoring network in the region (Parajuli et al. 2008; Nath and Thingbaijam 2011).
A database of strong ground-motion recordings released by Pacific Earthquake Engineering Research Center PEERR) is used to establish the models.
