Results 221 to 230 of about 19,474 (278)
Oceanic upper crustal accretion by melt sill and lava flow interaction at Axial volcano. [PDF]
Wu H +6 more
europepmc +1 more source
Integrating physics and machine learning for unified seismic forward modeling and reservoir property inversion. [PDF]
Zayier Y, Yalikun Y, Cheng Y, Yang D.
europepmc +1 more source
Amplitude Versus Angle (AVA) feature restoration in prestack gathers via dictionary learning. [PDF]
Gao Y +5 more
europepmc +1 more source
Directional adaptive mode total variation for seismic data denoising. [PDF]
Banjade TP +4 more
europepmc +1 more source
U-Trans: a foundation model for seismic waveform representation and enhanced downstream earthquake tasks. [PDF]
Saad OM, Chen Y, Alkhalifah T.
europepmc +1 more source
Seismic noise and gravity-gradient noise [PDF]
Gravity gradient noise is generated by mass density changes through fluctuating gravity fields. Ambient seismic noise generated by microseismism, wind or of antropogenic origin is a possible source of such fluctuations. This work gives an overview of the impact of seismic noise and gravity-gradient noise on existing gravitational-wave detectors, and ...
Grote, Hartmut +3 more
core +5 more sources
Ocean wave sources of seismic noise [PDF]
International audienceNoise with periods 3 to 10 s, ubiquitous in seismic records, is expected to be mostly generated by pairs of ocean wave trains of opposing propagation directions with half the seismic frequency.
Fabrice Ardhuin +2 more
exaly +2 more sources
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Some interesting seismic noises
SEG Technical Program Expanded Abstracts 1984, 1984ABSTRACT This paper suggests that the identification of seismic noise increases our ability to evaluate deeper drilling targets. Seismic noise, as illustrated in basic, unstacked data, is shown to contain clues which the seismic processor may use to improve the resolution of the seismic section.
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Bulletin of the Seismological Society of America, 1962
Abstract The seismic noise spectrum in the frequency range 0.5 to 31.5 cycles per second is presented graphically for a number of sites over a wide geographical range. Except for a small anomalous effect near 2 or 3 cycles per second, the ground particle motion curves are observed to decrease smoothly with increasing frequency at a rate ...
G. E. Frantti +2 more
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Abstract The seismic noise spectrum in the frequency range 0.5 to 31.5 cycles per second is presented graphically for a number of sites over a wide geographical range. Except for a small anomalous effect near 2 or 3 cycles per second, the ground particle motion curves are observed to decrease smoothly with increasing frequency at a rate ...
G. E. Frantti +2 more
openaire +1 more source

