2015
DOI: 10.1016/j.jappgeo.2015.03.016
|View full text |Cite
|
Sign up to set email alerts
|

The L-DVV method for the seismic signal extraction

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1

Citation Types

0
2
0

Year Published

2016
2016
2023
2023

Publication Types

Select...
4

Relationship

3
1

Authors

Journals

citations
Cited by 4 publications
(4 citation statements)
references
References 12 publications
0
2
0
Order By: Relevance
“…The horizontal axis of the scatter diagram corresponds to the DVV plot of the surrogate time series and the vertical axis corresponds to that of the original time series. Quantification of the delay vector variance (QDV) is defined as follows (Yu et al 2015):…”
Section: Time-varying Wl Tfpf Algorithm Based On the L-dvv Methodsmentioning
confidence: 99%
See 1 more Smart Citation
“…The horizontal axis of the scatter diagram corresponds to the DVV plot of the surrogate time series and the vertical axis corresponds to that of the original time series. Quantification of the delay vector variance (QDV) is defined as follows (Yu et al 2015):…”
Section: Time-varying Wl Tfpf Algorithm Based On the L-dvv Methodsmentioning
confidence: 99%
“…The iAAFT of the surrogate has the same probability density distribution and roughly the same power spectrum as the original time series, while the noise (such as white Gaussian noise) has a roughly even power spectrum (Gautama et al 2004b). The proposed delay vector variance method based on the straight line sequence (L-DVV) is essentially an extension of the DVV method (Yu et al 2015). The straight line sequence is selected as the surrogate time series, meaning that this method is extremely sensitive to random noise and is able to accurately distinguish between the seismic signal and noise, providing a basis for time-varying WL TFPF processing.…”
Section: Introductionmentioning
confidence: 99%
“…However, for intermediate frequency (around 40 Hz) seismic record discrimination, conventional TFPF would cause serious amplitude attenuation, even for the shortest window in PWVD (Wu et al, 2014). In other words, sometimes there is no guarantee of linearity (Yu et al, 2015) of the desired signal, even for extreme values of the parameter. The limitation of the conventional TFPF is that it views the signal only along the time direction where the rapid variation may cause serious distortion.…”
Section: Conventional Time-frequency Peak Filteringmentioning
confidence: 99%
“…In general, the effective signals in the microseismic records are often represented as the high-frequency reflection events with weak energy and short duration (Maxwell and Urbanic, 2001), (Shemeta and Anderson, 2010). Meanwhile, the recorded data is always contaminated by the intense background noise, bringing difficulty in extracting meaningful information (Yu et al, 2015), (Yu et al, 2016). Therefore, telling the desired signals from the unwanted noise has great significance in the microseismic data processing.…”
Section: Introductionmentioning
confidence: 99%