Caveats on tomographic images

Gillian R. Foulger; Giuliano F. Panza; Irina Artemieva; Ian D. Bastow; Fabio Cammarano; John R. Evans; Warren B. Hamilton; Bruce R. Julian; Michele Lustrino; Hans Thybo; Tatiana B. Yanovskaya

doi:10.1111/ter.12041

Caveats on tomographic images

Gillian R. Foulger, Giuliano F. Panza, Irina Artemieva, Ian D. Bastow, Fabio Cammarano, John R. Evans, Warren B. Hamilton, Bruce R. Julian, Michele Lustrino, Hans Thybo, Tatiana B. Yanovskaya

Geologi

78 Citationer (Scopus)

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Abstract

Geological and geodynamic models of the mantle often rely on joint interpretations of published seismic tomography images and petrological/geochemical data. This approach tends to neglect the fundamental limitations of, and uncertainties in, seismic tomography results. These limitations and uncertainties involve theory, correcting for the crust, the lack of rays throughout much of the mantle, the difficulty in obtaining the true strength of anomalies, choice of what background model to subtract to reveal anomalies, and what cross-sections to select for publication. The aim of this review is to provide a relatively non-technical summary of the most important of these problems, collected together in a single paper, and presented in a form accessible to non-seismologists. Appreciation of these issues is essential if final geodynamic models are to be robust, and required by the scientific observations.

Originalsprog	Engelsk
Tidsskrift	Terra Nova
Vol/bind	25
Udgave nummer	4
Sider (fra-til)	259-281
Antal sider	23
ISSN	0954-4879
DOI	https://doi.org/10.1111/ter.12041
Status	Udgivet - aug. 2013

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10.1111/ter.12041

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abstract = "Geological and geodynamic models of the mantle often rely on joint interpretations of published seismic tomography images and petrological/geochemical data. This approach tends to neglect the fundamental limitations of, and uncertainties in, seismic tomography results. These limitations and uncertainties involve theory, correcting for the crust, the lack of rays throughout much of the mantle, the difficulty in obtaining the true strength of anomalies, choice of what background model to subtract to reveal anomalies, and what cross-sections to select for publication. The aim of this review is to provide a relatively non-technical summary of the most important of these problems, collected together in a single paper, and presented in a form accessible to non-seismologists. Appreciation of these issues is essential if final geodynamic models are to be robust, and required by the scientific observations.",

author = "Foulger, {Gillian R.} and Panza, {Giuliano F.} and Irina Artemieva and Bastow, {Ian D.} and Fabio Cammarano and Evans, {John R.} and Hamilton, {Warren B.} and Julian, {Bruce R.} and Michele Lustrino and Hans Thybo and Yanovskaya, {Tatiana B.}",

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T1 - Caveats on tomographic images

AU - Foulger, Gillian R.

AU - Panza, Giuliano F.

AU - Artemieva, Irina

AU - Bastow, Ian D.

AU - Cammarano, Fabio

AU - Evans, John R.

AU - Hamilton, Warren B.

AU - Julian, Bruce R.

AU - Lustrino, Michele

AU - Thybo, Hans

AU - Yanovskaya, Tatiana B.

PY - 2013/8

Y1 - 2013/8

N2 - Geological and geodynamic models of the mantle often rely on joint interpretations of published seismic tomography images and petrological/geochemical data. This approach tends to neglect the fundamental limitations of, and uncertainties in, seismic tomography results. These limitations and uncertainties involve theory, correcting for the crust, the lack of rays throughout much of the mantle, the difficulty in obtaining the true strength of anomalies, choice of what background model to subtract to reveal anomalies, and what cross-sections to select for publication. The aim of this review is to provide a relatively non-technical summary of the most important of these problems, collected together in a single paper, and presented in a form accessible to non-seismologists. Appreciation of these issues is essential if final geodynamic models are to be robust, and required by the scientific observations.

AB - Geological and geodynamic models of the mantle often rely on joint interpretations of published seismic tomography images and petrological/geochemical data. This approach tends to neglect the fundamental limitations of, and uncertainties in, seismic tomography results. These limitations and uncertainties involve theory, correcting for the crust, the lack of rays throughout much of the mantle, the difficulty in obtaining the true strength of anomalies, choice of what background model to subtract to reveal anomalies, and what cross-sections to select for publication. The aim of this review is to provide a relatively non-technical summary of the most important of these problems, collected together in a single paper, and presented in a form accessible to non-seismologists. Appreciation of these issues is essential if final geodynamic models are to be robust, and required by the scientific observations.

U2 - 10.1111/ter.12041

DO - 10.1111/ter.12041

M3 - Journal article

SN - 0954-4879

VL - 25

SP - 259

EP - 281

JO - Terra Nova

JF - Terra Nova

IS - 4

ER -

Caveats on tomographic images

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