Mathematical model of seismic signal, as a flow of physically non realizable single seismic waves
Journal Title: Геофизический журнал - Year 2016, Vol 38, Issue 5
Abstract
The new conception of seismic data analysis is proposed. It is based on preliminary studying of seismic background. Its characteristics are a base for using mathematical models of non realizable seismic signals. The specific mathematical model of the seismic signal is proposed as well. The peculiarity of the model is that it allows you to simulate the flow of seismic waves of different classes each of them appears in the stream with specific time delay. This process takes place against the micro-seismic background noise. It is natural to model the flow of signals by the physically realizable signal. It means those signals which do not have a trace in prehistory. But this representation of the signal is unacceptable for two reasons. The first one is related to the smoothness of the signal at the time of its appearance on the seismic record. The second one is related to the fact that the fade of the signal in the noise does not allow us to determine the time of its appearance on the record accurately. The latter circumstance does not leave us the possibility to simulate the time of the signal occurrence by using the determined value. Therefore, the time of occurrence of the signal is simulated by random variable with variance depending on the level of micro-seismic background. We introduce the notion of generalized seismic signal as a function of time and of the vector of parameters, which determine its shape, the energy, the place in flow of the other signals, spectral characteristics, and in general behaviour in the entire history of its existence. Any widely spread seismic signal models used in practice are a particular case of this one. Or in a more rigorous approach to the definition the different particular cases of the signals classes are transformed into the different hyper-planes into space of parameters.
Authors and Affiliations
V. S. Mostovoy, S. V. Mostovyi
Periodization and specific features of deep processes in Precambrian by example of the Ukrainian shield
Thorough information on geological structure of the Ukrainian shield (USh) allows to verify opinions existing nowadays that plume and plate tectonic activities are possible only after conclusive formation of sublithosphe...
Stanislav Petrovich Ipatenko is 80
Stanislav Petrovich Ipatenko is 80
Dynamics of temporal changes of geomagnetic field secular variations
Time changes of the geomagnetic field secular variations, cleaned by three and eleven years running means were studying. The years of the changes of sign secular variations and years of the changes of their velocity wer...
Commentary on the article by H.H. Guliyev "Analysis of result of interpretation of elastic parameters of solid core of the Earth from the standpoint of current geomechanics"
Commentary on the article by H.H. Guliyev "Analysis of result of interpretation of elastic parameters of solid core of the Earth from the standpoint of current geomechanics"
Reflection of the history of consolidated Earth’s crust formaion of the Amur area gold-bearing province in its petrochemical composition (based on the data of seismic profiles Tynda—Amurset and Abakan—Tynda—Tatar channel)
Petrochemical sections along the stretches of geophysical profiles have been plotted based on the data of velocities of seismic waves propagation in consolidated crust, distribution of the main petrochemical types of roc...