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2.904  Articles
1 of 291 pages  |  10  records  |  more records»
In seismic exploration, random noise deteriorates the quality of acquired data. This study analyzed existing denoising methods used in seismic exploration from the perspective of random noise. Wavelet thresholding offers a new approach to reducing random ... see more

Seismic interface waves generated by seabed impacts are believed to have biological importance. Previous work on the effects of ocean piling and dredging studied water motion adjacent to the seabed, using sediment measurements as reviewed in the literatur... see more

Since 1996, the electric field strength of the two broadcasting stations MCO (f=216 kHz, southeast France) andCZE (f=270 kHz, Czech Republic) has been sampled every ten minutes by a receiver (AS) located in centralItaly. Here, we review the results obtain... see more

Relative wavelet energy entropy (RWEE) is proposed to detect and quantify damage to hysteretic dampers used for the passive seismic control of building structures. Hysteretic dampers have the role of dissipating most of the energy input of an earthquake. ... see more

Rayleigh wave detection is a recently developed method for shallow seismic exploration. Current Rayleigh wave data processing and interpretation methods can only provide the transverse average wave velocity of rock-soil bodies under the geophone array ran... see more

This study has been done to map the distribution of gas saturated sandstone reservoir by using stochastic seismic inversion in the “X” field, Bonaparte basin. Bayesian stochastic inversion seismic method is an inversion method that utilizes the principle ... see more

The development of Pre-stack depth migration makes the imaging of the subsurface structure in the depth possible, which set a foun- dation for the study of amplitude variation with incident angle (AVA) inversion. This leads to the increasing demanding of ... see more

The East Java Basin is developed from an oceanic basin in front of Late Cretaceous Java Trench subduction zone to presently back-arc basin behind the Java-Lombok volcanic arc to the south. Many studies conclude hydrocarbon discovery in deep carbonate Ngim... see more

The East Java Basin is developed from an oceanic basin in front of Late Cretaceous Java Trench subduction zone to presently back-arc basin behind the Java-Lombok volcanic arc to the south. Many studies conclude hydrocarbon discovery in deep carbonate Ngim... see more

1 of 291 pages  |  10  records  |  more records»