Results 31 to 40 of about 1,357,139 (273)
Seismic random noise suppression using improved CycleGAN
Random noise adversely affects the signal-to-noise ratio of complex seismic signals in complex surface conditions and media. The primary challenges related to processing seismic data have always been reducing the random noise and increasing the signal-to-
Shimin Sun +8 more
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Denoising of Seismic Data Based on Block Dictionary Learning Theory
With the increasingly complex observation environment of oil and gas exploration, the seismic data collected are often mixed with various noise signals, resulting in the effective weak signal caused by the exploration target is covered, which seriously ...
Junjie ZHOU +3 more
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Interferometric surface-wave isolation and removal [PDF]
The removal of surface waves (ground roll) from land seismic data is critical in seismic processing because these waves tend to mask informative body-wave arrivals.
Robertsson, Johan O. A. +3 more
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Multi-scale interactive network in the application of DAS seismic data processing
Distributed acoustic sensing (DAS) is regarded as a novel acquisition technology for seismic data. Compared with conventional electrical geophones, DAS has a series of obvious advantages including low-cost, high spatial resolution, good coverage, and ...
Hongzhou Wang +5 more
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OSG-057 Superconducting Gravimeter Noise Levels in Lhasa (China)
This research tests OSG-057 superconducting gravimeter (SG) performance in Lhasa in terms of noise levels in the seismic (2 min to 1 h), sub-seismic (1 to 6 h), and tidal (above 6 h) bands. Based on the Seismic Noise Magnitude (SNM) and Sub-Seismic Noise
Miaomiao Zhang +4 more
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Seismic and Newtonian Noise in the GW Detectors
Gravitational wave detectors aim to measure relative length variations of the order of ΔL/L≃10−21, or less. Thus, any mechanism that is able to reproduce such a tiny variation can, in principle, threaten the sensitivity of these instruments, representing
Lucia Trozzo, Francesca Badaracco
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Seismic noise between 0.003 Hz and 1.0 Hz and its classification
It is now established that the primary microseism, the secondary microseisms, and the hum are the three main components of seismic noise in the frequency band from about 0.003 Hz to 1.0 Hz. Monthly averages of seismic noise are dominated by these signals
Toshiro Tanimoto, Aaron Anderson
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Characterization of the temporal and spatial distribution of ambient seismic noise in an urban site
reservedambient seismic noise characterization is an advanced look at the subsurface and its importance for many disciplines such as oil exploration, geology, earthquake engineering, hydrology and structural health monitoring made it the focus of many ...
ELGASHTI, MOHAMED AMER ALI
core
Passive seismic interferometry is a technique that reconstructs virtual seismic records using ambient noise, such as random noise or microseisms. The ambient noise in passive seismic data contains rich information, with surface waves being useful for the
Xiaolong Li +3 more
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Quantifying the response of human activity to different COVID-19 measures may serve as a potential way to evaluate the effectiveness of the measures and optimize them.
Junzhu Shen, Tieyuan Zhu
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