scholarly journals Seismic characteristics of the structures at variation of artificial accelerograms

Author(s):  
Stjepan Lakusic
1995 ◽  
Author(s):  
Theron J. Bennett ◽  
Keith L. McLaughlin ◽  
Margaret E. Marshall ◽  
Brian W. Barker ◽  
John R. Murphy

Author(s):  
GENE F. SIRCA ◽  
HOJJAT ADELI

In earthquake-resistant design of structures, for certain structural configurations and conditions, it is necessary to use accelerograms for dynamic analysis. Accelerograms are also needed to simulate the effects of earthquakes on a building structure in the laboratory. A new method of generating artificial earthquake accelerograms is presented through adroit integration of neural networks and wavelets. A counterpropagation (CPN) neural network model is developed for generating artificial accelerograms from any given design spectrum such as the International Building Code (IBC) design spectrum. Using the IBC design spectrum as network input means an accelerogram may be generated for any geographic location regardless of whether earthquake records exist for that particular location or not. In order to improve the efficiency of the model, the CPN network is modified with the addition of the wavelet transform as a data compression tool to create a new CPN-wavelet network. The proposed CPN-wavelet model is trained using 20 sets of accelerograms and tested with additional five sets of accelerograms available from the U.S. Geological Survey. Given the limited set of training data, the result is quite remarkable.


1976 ◽  
Vol 66 (6) ◽  
pp. 1953-1964 ◽  
Author(s):  
William Stauder ◽  
Mark Kramer ◽  
Gerard Fischer ◽  
Stephen Schaefer ◽  
Sean T. Morrissey

abstract A regional microearthquake network has been established in the New Madrid seismic zone to study better the seismic characteristics of this region. The network consists of 16 stations distributed on the borders of and within the head of the Mississippi embayment. The network has a location sensitivity for all earthquakes of mb ≧ 1 occurring within the network. A total of 330 earthquakes has been located within a 1.5° by 1.5° area inside the array during the first 21 months of operation. The spatial distribution of these hypocenters has identified for the first time in this region the existence of linear seismically active zones, corresponding presumably to seismically active faults. Several of these trend N40°E, parallel to the axis of the embayment. Others trend NW; these latter are parallel to and possibly are related to the crest of the Pascola arch which joins the Ozark uplift to the Nashville dome. The linear dimensions of the features identified thus far vary in length from about 25 km to about 100 km. The b value as determined by the number of earthquakes located thus far is about 0.8.


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