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1-20 OF 23 RESULTS FOR
Riesz Transform
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Journal Article
Edge detection of potential-field sources using scale-space monogenic signal: Fundamental principles
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 24 July 2015
Geophysics (2015) 80 (5): J27–J36.
... the vertical component f z of a conservative field F , the x - and y -components of the first-order Riesz transform of f z were the horizontal components f x and f y of F . Hence, the local amplitude of the monogenic signal of f z is the 3D analytic signal amplitude of the scalar potential of F and the local...
Image
Schematic representation of monogenic signal vector m (equation 7 ...
in Edge detection of potential-field sources using scale-space monogenic signal: Fundamental principles
> Geophysics
Published: 24 July 2015
Figure 1. Schematic representation of monogenic signal vector m (equation 7 ) in 3D Euclidean space. The component f ≡ f ( x , y ) is the signal, and the components r x and r y are the x - and y -components of the first-order Riesz
Image
Concepts and relationships of (a) the magnetic field, (b) the 2D horizontal...
in Attributes of the magnetic field, analytic signal, and monogenic signal for gravity and magnetic interpretation
> Geophysics
Published: 10 October 2016
of the monogenic signal are the two first-order Riesz transforms, i.e., the x - and y -derivatives of the vertical integral of the input function f ( x , y ) . See Table 1 for the definition of the input function and the components of the 2D and 3D vectors in each of the three cases
Journal Article
Attributes of the magnetic field, analytic signal, and monogenic signal for gravity and magnetic interpretation
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 10 October 2016
Geophysics (2016) 81 (6): J79–J86.
... of the monogenic signal are the two first-order Riesz transforms, i.e., the x - and y -derivatives of the vertical integral of the input function f ( x , y ) . See Table 1 for the definition of the input function and the components of the 2D and 3D vectors in each of the three cases...
Journal Article
The monogenic signal of potential-field data: A Python implementation
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 06 March 2017
Geophysics (2017) 82 (3): F9–F14.
... . In this particular case, the three components of the monogenic signal will be given by the original data function, and its first-order Riesz transform; i.e., M NS ( u , v ) = [ F i u u 2 + v 2 F i v u 2 + v 2 F ] . (7...
Series: Society of Exploration Geophysicists Geophysical References Series
Publisher: Society of Exploration Geophysicists
Published: 16 November 2022
DOI: 10.1190/1.9781560803874.chr
EISBN: 978-1-56080-387-4
... Euler deconvolution . Riesz transform: generalization of the one-dimensional (1D) Hilbert transform for dimensions D ≥ 2. A two-dimensional (2D) Riesz transform adds to an anomalous field two quadrature , or mutually orthogonal, field components obtained by two 90° phase shifts at each...
Journal Article
Multiscale Analysis of Hydrologic Time Series Data using the Hilbert–Huang Transform All rights reserved. No part of this periodical may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying, recording, or any information storage and retrieval system, without permission in writing from the publisher.
Journal: Vadose Zone Journal
Publisher: Soil Science Society of America
Published: 01 November 2010
Vadose Zone Journal (2010) 9 (4): 925–942.
... efficiency, which is mandatory, in particular, for multisensorial data in several space dimensions. Moreover, the second step, the Hilbert transform, also needed to be generalized to extend the analytical signals to arbitrary dimensions. Based on ideas using Clifford algebra and Riesz transforms from...
Journal Article
The asymptotic local finite-difference method of the fractional wave equation and its viscous seismic wavefield simulation
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 16 April 2020
Geophysics (2020) 85 (3): T179–T189.
...., 2013 ; Zhu and Harris, 2014 ). Many numerical methods are used to study the viscosity of wave absorption and attenuation with the fractional-order seismic wave equation. When m = 2 , the average of three points from equation 7 is approximated as the Riesz derivative and a fourth-order...
Journal Article
Adaptive wavelets for analyzing dispersive seismic waves
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 16 November 2006
Geophysics (2007) 72 (1): V1–V11.
... and Van Loan, 1983 ; Riesz and Nagy, 1955 ; Aster et al., 2005 ). This approach has proven to be very useful in climate dynamics and other areas ( Vautard and Ghil, 1989 ; Yiou et al., 2000 ). Our choice of the KL transform is based on the concept of minimizing the average approximate error according...
Series: Society of Exploration Geophysicists Geophysical References Series
Publisher: Society of Exploration Geophysicists
Published: 16 November 2022
DOI: 10.1190/1.9781560803874.chjkl
EISBN: 978-1-56080-387-4
... imaginary, or 90° phase -shifted, parts obtained by Riesz transform of f ( x , y ) in the orthogonal complex planes (Felsberg and Sommer, 2001). Because the Riesz transform operators R 1 and R 2 are equivalent to the x - and y -components H x and H y of the 3D Hilbert transform...
Journal Article
Identifying the lithology of volcanic rocks by using the time-frequency features of array acoustic logging data
Journal: Interpretation
Publisher: Society of Exploration Geophysicists
Published: 01 July 2020
Interpretation (2020) 8 (3): SL127–SL136.
..., frequencies, or amplitudes, we have analyzed the array acoustic logging signals by the fractional Fourier transform and the Choi-Williams distribution. First, we apply the fractional Fourier transform on an array acoustic logging waveform with proper α , then the Choi-Williams distribution analysis method...
Journal Article
3-D magnetic inversion with data compression and image focusing
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 01 January 2002
Geophysics (2002) 67 (5): 1532–1541.
..., the conjugate gradient method can be applied even in this case. For an underdetermined problem (where N m > N d ), the conjugate gradient iterations (6) converge to the minimum norm solution m min : (8) Expression (8) is also known as the Riesz representation formula ( Parker, 1994...
Journal Article
Robust estimation of structural orientation parameters and 2D/3D local anisotropic Tikhonov regularization
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 03 October 2024
Geophysics (2024) V521–V536.
... = h z ⋆ m , (33) with the generalized 3D Hilbert (Riesz) transform filters: h x = − 1 π 2 x ( x 2 + y 2 + z 2 ) 2 , h y = − 1 π 2 y ( x 2 + y 2 + z 2 ) 2...
Series: Society of Exploration Geophysicists Geophysical References Series
Publisher: Society of Exploration Geophysicists
Published: 16 November 2022
DOI: 10.1190/1.9781560803874.chm
EISBN: 978-1-56080-387-4
... phase of monogenic signal (MS). monogenic signal (MS): 1. representation of a scalar anomalous gravity or magnetic field by means of a three-component vector derived from the Riesz transform , which augments the anomalous field by the addition of two mutually orthogonal field components...
Journal Article
A matrix-transform numerical solver for fractional Laplacian viscoacoustic wave equation
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 19 June 2019
Geophysics (2019) 84 (4): T283–T297.
...Hanming Chen; Hui Zhou; Ying Rao; Pengyuan Sun; Jianlei Zhang; Yangkang Chen ABSTRACT We have developed a matrix-transform method (MTM) to numerically solve the fractional Laplacian constant- Q viscoacoustic wave equation. The new method is based on a matrix representation of the fractional...
Series: Society of Exploration Geophysicists Geophysical References Series
Publisher: Society of Exploration Geophysicists
Published: 16 November 2022
DOI: 10.1190/1.9781560803874.chh
EISBN: 978-1-56080-387-4
...” and “imaginary” parts, where the real part represents the original data and the imaginary part is the 90° phase-shifted real part. The imaginary part of the complex variable obtained by the Hilbert transform is also referred to as quadrature or quadrature signal . See also Riesz transform , 3D Hilbert...
Series: Society of Exploration Geophysicists Geophysical References Series
Publisher: Society of Exploration Geophysicists
Published: 16 November 2022
DOI: 10.1190/1.9781560803874.chf
EISBN: 978-1-56080-387-4
... ; and (2) inverse Fourier transform, which converts the Fourier-transformed data back to their original space domain . Sometimes referred to as spectral transform . See also discrete Fourier transform (DFT) , window Fourier transform (WFT) , Hilbert transform , Riesz transform , and Walsh...
Series: Society of Exploration Geophysicists Geophysical References Series
Publisher: Society of Exploration Geophysicists
Published: 16 November 2022
DOI: 10.1190/1.9781560803874.chpq
EISBN: 978-1-56080-387-4
... transform and Riesz transform . quadrature filters: a pair of filters which have the same frequency response but differ in phase by 90°. See also filter and steerable filter . quadrature pair: Hilbert transform pair in the context of a pair of functions which are in quadrature...
Series: Society of Exploration Geophysicists Geophysical References Series
Publisher: Society of Exploration Geophysicists
Published: 16 November 2022
DOI: 10.1190/1.9781560803874.chc
EISBN: 978-1-56080-387-4
... representing the odd (sine) and even (cosine) components in Fourier-transformed data and comprise a Hilbert transform pair , wherein the imaginary part is the 90° phase -shifted real part. See also Fourier transform , sine transform , cosine transform , and Riesz transform . complex monogenic signal...
Series: Society of Exploration Geophysicists Geophysical References Series
Publisher: Society of Exploration Geophysicists
Published: 16 November 2022
DOI: 10.1190/1.9781560803874.chd
EISBN: 978-1-56080-387-4
... signal (MS) . It is composed of two imaginary parts obtained from the real part of the MS by the first-order Riesz transform operators R 1 and R 2 and projected on the direction of the monogenic signal orientation. It is expressed as H θ = R 1 f ( x , y ) cos θ + R 2 f...
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