Semi-automatic interpretation methods for extracting structural boundaries using gravity gradient tensors
Author:
Affiliation:
1. Graduate School of Science and Engineering for Research (Science), University of Toyama
Publisher
Society of Exploration Geophysicists of Japan
Subject
General Engineering
Link
https://www.jstage.jst.go.jp/article/segj/69/1/69_53/_pdf
Reference42 articles.
1. Beiki, M. (2010): Analytic signals of gravity gradient tensor and their application to estimate source location, Geophysics, 75, I59-I74.
2. Beiki, M. (2013): TSVD analysis of Euler deconvolution to improve estimating magnetic source parameters: an example from the Asele area, Sweden, Jour. Appl. Geophys., 90, 82-91.
3. Beiki, M., and Pedersen, L. B. (2010): Eigenvector analysis of gravity gradient tensor to locate geologic bodies, Geophysics, 75, I37-I49.
4. Blakely, R. and Simpson, R. W. (1986): Approximating edges of source bodies from magnetic or gravity anomalies, Geophysics, 51, 1494-1498.
5. Bott, M. H. P. (1962): A simple criterion for interpreting negative gravity anomalies, Geophysics, 27, 376-381.
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1. Continuity, segmentation and faulting type of active fault zones of the 2016 Kumamoto earthquake inferred from analyses of a gravity gradient tensor;Earth, Planets and Space;2016-10-21
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