نتایج جستجو برای: x domain seismic gathers

تعداد نتایج: 1043226  

2005
Gabriel Alvarez

Wave-equation migration with the velocity of the primaries maps non-diffracted waterbottom multiples to an hyperbola in subsurface-offset-domain-common-image-gathers. Furthermore, for positive surface offsets, the multiples are mapped to non-positive subsurface offsets if sediment velocity is faster than water. The larger the offset in the data space, the larger the subsurface offset and the sh...

2005
E. Landa S. Fomel T. J. Moser

A B S T R A C T A new type of seismic imaging, based on Feynman path integrals for waveform modelling , is capable of producing accurate subsurface images without any need for a reference velocity model. Instead of the usual optimization for traveltime curves with maximal signal semblance, a weighted summation over all representative curves avoids the need for velocity analysis, with its common...

2013
Kiran Khonde Richa Rastogi

This paper presents a review of spectral decomposition of seismic data, since it's inception nearly in 1997. It discusses various techniques and applications of spectral decomposition in seismic data processing and interpretation. It is also known as timefrequency analysis consists of transforming non stationary signal in time/space from time/space domain to time/space vs frequency domain. The ...

Journal: :Solid Earth 2022

Abstract. Accurate subsurface velocity models are crucial for geological interpretations based on seismic depth images. Seismic reflection tomography is an effective iterative method to update and refine a preliminary model imaging. Based residual move-out analysis of reflectors in common image point gathers, the estimated by ray-based tomography. To stabilize tomography, several preconditionin...

2005
Biondo Biondi

To enable the analysis of the Residual Moveout (RMO) in Angle-Domain Common Image Gathers (ADCIGs) after anisotropic wavefield-continuation migration, I develop the fundamental concepts for quantitatively relating perturbations in anisotropic parameters to the corresponding reflector movements in ADCIGs. I then apply the general methodology to the particular case of RMO analysis of reflections ...

2016
Marion Gilson M. Gilson

This paper gathers several experiences of using instrumental variable method in different contexts: closed-loop system identification, LPV model, frequency domain framework.

Journal: :Frontiers in Earth Science 2023

Imaging of multiples, as a supplement to imaging primaries, can provide wider range subsurface illumination. Therefore, it more detailed information on structures. However, multiples suffers from crosstalk issues generated by unrelated events. Many strategies have been proposed attenuate crosstalk, among which the angle domain Radon attenuation algorithm achieves good application effect. In dom...

Journal: :civil engineering infrastructures journal 0
masood heshmati k. n. toosi university of technology mohammad amin hariri ardebili university of colorado ar boulder hasan mirzabozorg k. n. toosi university of technology seyed mahdi seyed kolbadi k. n. toosi university of technology

differences between stress-based and strain-based criteria are investigated in seismic performance evaluation of the arch dams in time domain. a numerical model of the coupled dam-reservoir-foundation system is prepared with the finite element technique. reservoir is modeled using the eulerian approach as a compressible domain, and the foundation rock is assumed to be massless. dynamic equilibr...

Journal: :فیزیک زمین و فضا 0
ایمان گنجی دانشجوی دکتری ژئوفیزیک، گروه ژئوفیزیک، دانشگاه آزاد اسلامی، واحد علوم و تحقیقات حمیدرضا سیاهکوهی دانشیار، گروه فیزیک زمین، مؤسسة ژئوفیزیک دانشگاه

seismic waves travelling through inelastic media are attenuated by the conversion of elastic energy into heat. upon being attenuated, the travelling wave changes: amplitude is reduced, travelling waveform is modified due to high-frequency content absorption, and phase is delayed. attenuation is usually quantified through the quality factor q: the ratio between the energy stored and lost in each...

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