2017
DOI: 10.1016/j.physa.2017.02.029
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Heterogeneity analysis of geophysical well-log data using Hilbert–Huang transform

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Cited by 22 publications
(6 citation statements)
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“…The whole process is an adaptive process, fully data-driven, without the need to define functions in advance. The main steps of EMD are as follows [159][160][161][162][163][164][165]:…”
Section: Theorymentioning
confidence: 99%
See 1 more Smart Citation
“…The whole process is an adaptive process, fully data-driven, without the need to define functions in advance. The main steps of EMD are as follows [159][160][161][162][163][164][165]:…”
Section: Theorymentioning
confidence: 99%
“…The EMD decomposition process is shown in Figure 14: [159][160][161] An example of EMD decomposition is shown in Figure 15: The existing body of research on EMD suggests that it is a powerful decomposition tool in time series analysis. Therefore, EMD is usually combined with other methods for data processing.…”
Section: Theorymentioning
confidence: 99%
“…By integrating the Hilbert spectrum, the energy spectrum could be well obtained, which can be used to analyze the energy distribution of vibration signals varied with time and frequency. It breaks the limitation of the uncertainty principle and can accurately express all kinds of information on the time-frequency plane [22,23].…”
Section: Introductionmentioning
confidence: 99%
“…While wavelet analysis still requires one to choose basis functions, the Hilbert–Huang Transform (HHT) introduced by [ 14 ] is truly data adaptive and therefore, well suited for the analysis of general time series of unknown origin that include non-stationarity. HHT, and its fundamental engine, the Empirical Mode Decomposition (EMD), have become a widely used tool to analyze time series measurements that perform equally well for stationary as for non-stationary signals, e.g., [ 15 , 16 , 17 , 18 ]. Whether or not non-stationary signals should be removed from time series for HVSR processing is still debated between authors who consider it necessary to exclude spikes and transients in microtremors, e.g., [ 19 , 20 , 21 ] who suggest that non-stationary large amplitude noise windows should not be removed, because these can carry subsoil information, potentially improving the correlation between noise and earthquakes in HVSR curves.…”
Section: Introductionmentioning
confidence: 99%