Relationship between the average depth of a stratum boundary and the power spectrum of the g<sub>zz</sub> component of a gravity gradient tensor-Reference-Cited by-同舟云学术

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Relationship between the average depth of a stratum boundary and the power spectrum of the g_zz component of a gravity gradient tensor

Published:2017 Issue:0 Volume:70 Page:1-11
ISSN:0912-7984
Container-title:BUTSURI-TANSA(Geophysical Exploration)
language:en
Short-container-title:BUTSURI-TANSA(Geophysical Exploration)

Author:

Kusumoto Shigekazu¹,Higashinaka Motonori²

Affiliation:

1. Graduate School of Science and Engineering for Research(Science), University of Toyama

2. JGI, Inc

Publisher

Society of Exploration Geophysicists of Japan

Subject

General Engineering

Link

https://www.jstage.jst.go.jp/article/segj/70/0/70_1/_pdf

Reference17 articles.

1. Barnes, G., and Barraud, J. (2012): Imaging geologic surfaces by inverting gravity gradient data with depth horizons, Geophysics, 77, G1-G11.

2. Beiki, M., and Pedersen, L. B. (2010): Eigenvector analysis of gravity gradient tensor to locate geologic bodies, Geophysics, 75, I37-I49.

3. Blakely, R. J. (1996): Potential theory in gravity and magnetic applications, Cambridge University Press, Cambridge.

4. Bracewell, R. (1965): The Fourier transform and its applications, McGraw-Hill, New York.

5. Braga, M. A., Endo, I., Galbiatti, H. F., and Carlos, D. U. (2014): 3D full tensor gradiometry and Falcon systems data analysis for iron ore exploration: Bau Mine, Quadrilatero Ferrifero, Minas Gerais, Brazil, Geophysics, 79, B213-B220.

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