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all geography including DSDP/ODP Sites and Legs
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Africa
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Afar (1)
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East Africa
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Tanzania
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Olduvai Gorge (1)
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Nile River (1)
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North Africa
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Egypt
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Morocco
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Southern Africa
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West Africa (1)
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Antarctica
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Arctic Ocean
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Southern Europe
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Iberian Peninsula
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Spain
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Italy
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Campania Italy
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Western Europe
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France
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Isere France
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Indian Ocean
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Malay Archipelago
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Mexico
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North America
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Appalachians (2)
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Basin and Range Province
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Canadian Shield
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Gulf Coastal Plain (1)
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Western Canada Sedimentary Basin (1)
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North Island (1)
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Oceania
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Melanesia
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Vanuatu (1)
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Polynesia
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Hawaii
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Hawaii County Hawaii
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Kilauea (1)
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Tonga (1)
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Pacific Ocean
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East Pacific
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North Pacific
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Tertiary
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middle Oligocene (1)
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upper Oligocene (2)
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Lake Bonneville (1)
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Mesozoic
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Primary terms
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absolute age (2)
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Africa
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Afar (1)
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East Africa
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Tanzania
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Olduvai Gorge (1)
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Nile River (1)
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North Africa
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Algeria (3)
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Egypt
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Journal Article
Source-independent seismic envelope inversion based on the direct envelope Fréchet derivative Available to Purchase
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 01 October 2018
Geophysics (2018) 83 (6): R581–R595.
...Pan Zhang; Ru-Shan Wu; Liguo Han ABSTRACT Seismic envelope inversion (EI) uses low-frequency envelope data to recover long-wavelength components of the subsurface media. Conventional EI uses the same waveform Fréchet derivative as conventional full-waveform inversion. Due to linearization...
Journal Article
Fast 2D inversion of large borehole EM induction data sets with an efficient Fréchet-derivative approximation Available to Purchase
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 31 December 2008
Geophysics (2009) 74 (1): E75–E91.
... validated a new inversion method to estimate 2D parametric spatial distributions of electrical resistivity from array-induction measurements acquired in a vertical well. The central component of the method is an efficient approximation to Fréchet derivatives where both the incident and adjoint fields...
Journal Article
Fast Frechet derivative calculation using an auxiliary source array method: An application to array resistivity measurements Available to Purchase
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 01 January 2001
Geophysics (2001) 66 (5): 1364–1371.
...Tsili Wang; Alberto Mezzatesta Abstract Frechet derivatives provide the vital information for parametric resistivity inversion, but the calculation for a multidimensional problem is often computer intensive. This paper presents a new technique for fast calculation of the Frechet derivatives...
Journal Article
Approximate Frechet derivatives in inductive electromagnetic soundings Available to Purchase
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 01 December 1990
Geophysics (1990) 55 (12): 1589–1595.
...David E. Boerner; J. S. Holladay Abstract Frechet derivatives play dual roles in electromagnetic (EM) methods as averaging functions relating conductivity to EM fields and as sensitivity functions relating conductivity perturbations to changes in these fields. For one-dimensional EM inductive...
Journal Article
Explicit expressions for the Fréchet derivatives in 3D anisotropic resistivity inversion Available to Purchase
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 10 April 2009
Geophysics (2009) 74 (3): F31–F43.
...S. A. Greenhalgh; B. Zhou; M. Greenhalgh; L. Marescot; T. Wiese Abstract We have developed explicit expressions for the Fréchet derivatives or sensitivity functions in resistivity imaging of a heterogeneous and fully anisotropic earth. The formulation involves the Green's functions...
Journal Article
On the computation of the Fréchet derivatives for seismic waveform inversion in 3D general anisotropic, heterogeneous media Available to Purchase
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 28 September 2009
Geophysics (2009) 74 (5): WB153–WB163.
...Bing Zhou; Stewart Greenhalgh Abstract We present a perturbation method and a matrix method for formulating the explicit Fréchet derivatives for seismic body-wave waveform inversion in 3D general anisotropic, heterogeneous media. Theoretically, the two methods yield the same explicit formula valid...
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The rms sum of the Fréchet derivative using the (a) TT model (Figure 18a )... Available to Purchase
in Early arrival waveform inversion using data uncertainties and matching filters with application to near-surface seismic refraction data
> Geophysics
Published: 31 October 2022
Figure 24. The rms sum of the Fréchet derivative using the (a) TT model (Figure 18a ) and (b and c) EAWI-MF-DU final model (Figure 21g ). The maximum time window T used in Fréchet derivative calculation is depicted in the text boxes. Higher values indicate better constraint of the velocity
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Longitudinal conductivity Fréchet derivative d G ∕ d σ l var... Available to Purchase
in Explicit expressions for the Fréchet derivatives in 3D anisotropic resistivity inversion
> Geophysics
Published: 10 April 2009
Figure 4. Longitudinal conductivity Fréchet derivative d G ∕ d σ l variations in the subsurface for an anisotropic model having longitudinal conductivity of 0.1 S ∕ m , transverse conductivity of 0.025 S ∕ m , and strike of the symmetry axis of 0°. The various
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Fréchet derivative d G ∕ d σ t plots at the surface ( z... Available to Purchase
in Explicit expressions for the Fréchet derivatives in 3D anisotropic resistivity inversion
> Geophysics
Published: 10 April 2009
Figure 7. Fréchet derivative d G ∕ d σ t plots at the surface ( z = 0 ) for the same model and electrode configuration as in Figure 6 . All patterns are symmetrical about the x -axis. In the case of zero dip, the sensitivity is zero.
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Fréchet derivative d G ∕ d σ for an isotropic model having a co... Available to Purchase
in Explicit expressions for the Fréchet derivatives in 3D anisotropic resistivity inversion
> Geophysics
Published: 10 April 2009
Figure 3. Fréchet derivative d G ∕ d σ for an isotropic model having a conductivity of 0.1 S ∕ m . The current source is at (5,0,0) and the potential electrode is at (10,0,0). (a) The cross-sectional view at y = 0 and two horizontal depth slices at (b) z = 0
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Transverse conductivity Fréchet derivative d G ∕ d σ t varia... Available to Purchase
in Explicit expressions for the Fréchet derivatives in 3D anisotropic resistivity inversion
> Geophysics
Published: 10 April 2009
Figure 6. Transverse conductivity Fréchet derivative d G ∕ d σ t variations for the same anisotropic model and electrode configuration as in Figure 4 . The various sensitivity plots are for differing dips of the symmetry axis, as indicated. The profiles are perpendicular
Image
Fréchet derivative d G ∕ d σ l plots at the surface ( z... Available to Purchase
in Explicit expressions for the Fréchet derivatives in 3D anisotropic resistivity inversion
> Geophysics
Published: 10 April 2009
Figure 5. Fréchet derivative d G ∕ d σ l plots at the surface ( z = 0 ) for the same model and electrode configuration as Figure 4 . Note the symmetry of the plots and the decrease in sensitivity with increasing dip.
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Velocity model for comparing the analytic Fréchet derivative with the numer... Available to Purchase
Published: 22 March 2005
Figure 1. Velocity model for comparing the analytic Fréchet derivative with the numerical Fréchet derivative.
Image
Comparison of the analytic and numerical Fréchet derivative of traveltime, ... Available to Purchase
Published: 22 March 2005
Figure 2. Comparison of the analytic and numerical Fréchet derivative of traveltime, where the shot is located at (a) 1.5 km, (b) 2.5 km, and (c) 4.5 km, respectively. FDM = finite-difference method.
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Comparison of the analytic and numerical Fréchet derivative of amplitude wh... Available to Purchase
Published: 22 March 2005
Figure 3. Comparison of the analytic and numerical Fréchet derivative of amplitude where the shot is located at (a) 1.5 km, (b) 2.5 km, and (c) 4.5 km, respectively. FDM = finite-difference method.
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The 3-D sensitivity function (Frechét derivative) of normalised apparent re... Available to Purchase
Published: 01 January 2002
F IG . 12. The 3-D sensitivity function (Frechét derivative) of normalised apparent resistivity for the pole-pole array with a pole-pole distance of 1 m presented as horisontal depth slices at z = 0.01, 0.25, 0.5, 0.75, 1.0, and 1.5 m. The electrodes are located at (−0.5, 0, 0) m and (0.5, 0, 0
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2-D form of the Fréchet derivative for an electrode configuration with curr... Available to Purchase
Published: 01 January 2001
F IG . 2. 2-D form of the Fréchet derivative for an electrode configuration with current and potential electrodes placed at x = −15 m ( A ), x = 15 m ( B ), x = −25 m ( M ), and x = 45 m ( N ) (configuration s6 in Figure 4 ). Light gray indicates negative values; dark gray, positive
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The Frechet derivatives with respect to R xo in the layer between 60.9... Available to Purchase
in Fast Frechet derivative calculation using an auxiliary source array method: An application to array resistivity measurements
> Geophysics
Published: 01 January 2001
F IG . 4. The Frechet derivatives with respect to R xo in the layer between 60.96 and 63.40 m. The first track shows the model resistivity variations in depth. The shaded area in the second track shows the location of the invasion zone for which the Frechet derivatives are shown. The third
Journal Article
Refraction traveltime tomography using damped monochromatic wavefield Available to Purchase
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 22 March 2005
Geophysics (2005) 70 (2): U1–U7.
...Figure 1. Velocity model for comparing the analytic Fréchet derivative with the numerical Fréchet derivative. ...
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Fréchet derivatives computed from the Green’s functions in Figure 8 . Available to Purchase
in A low-rank approximation for large-scale 3D controlled-source electromagnetic Gauss-Newton inversion
> Geophysics
Published: 19 April 2016
Figure 9. Fréchet derivatives computed from the Green’s functions in Figure 8 .
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