TY - JOUR
T1 - TODGINV-A code for optimization of gravity anomalies due to anticlinal and synclinal structures with parabolic density contrast
AU - Chakravarthi, V.
AU - Sundararajan, N.
N1 - Funding Information:
The authors sincerely thank the Editor and the two anonymous reviewers for their critical reviews of the manuscript and constructive suggestions to improve the manuscript as presented here. Dr. V.P. Dimri, Director, National Geophysical Research Institute, Hyderabad, is gratefully acknowledged for his encouragement and permission to publish this work. V.C. acknowledges the Council of Scientific & Industrial Research (CSIR), Government of India, for financial support under the Young Scientist Award project.
PY - 2008/8
Y1 - 2008/8
N2 - A code, TODGINV, to determine the parameters of 2D anticlinal and synclinal structures besides estimating linear regional gravity background is presented wherein the density contrast varies with depth based on a parabolic equation. The main program, TODGINV, is supported by five subroutines namely GANTCLINE, GSYNCLINE, PDSANT, PDSSYN and NOREQS. Forward modeling is realized through the subroutine GANTCLINE in case of an anticlinal structure while GSYNCLINE in case of a synclinal structure. PDSANT and PDSSYN compute the partial derivatives of anticlinal and synclinal structures, respectively, whereas NOREQS solves the system of normal equations. The efficiency of the code is illustrated with a set of synthetic gravity anomalies over an anticlinal and a synclinal structure both with and without regional background. Further, the code is exemplified with the gravity anomalies of the Pays De Bray anticline, France, and the results are found to be more consistent with borehole information rather than with those of Alessandrello et al. (1983, Automatic three-layer, three-dimensional deconvolution of the Pays De Bray anticline. Geophysical Prospecting 31, 608-626).
AB - A code, TODGINV, to determine the parameters of 2D anticlinal and synclinal structures besides estimating linear regional gravity background is presented wherein the density contrast varies with depth based on a parabolic equation. The main program, TODGINV, is supported by five subroutines namely GANTCLINE, GSYNCLINE, PDSANT, PDSSYN and NOREQS. Forward modeling is realized through the subroutine GANTCLINE in case of an anticlinal structure while GSYNCLINE in case of a synclinal structure. PDSANT and PDSSYN compute the partial derivatives of anticlinal and synclinal structures, respectively, whereas NOREQS solves the system of normal equations. The efficiency of the code is illustrated with a set of synthetic gravity anomalies over an anticlinal and a synclinal structure both with and without regional background. Further, the code is exemplified with the gravity anomalies of the Pays De Bray anticline, France, and the results are found to be more consistent with borehole information rather than with those of Alessandrello et al. (1983, Automatic three-layer, three-dimensional deconvolution of the Pays De Bray anticline. Geophysical Prospecting 31, 608-626).
KW - Anticline
KW - Gravity anomaly
KW - Optimization
KW - Parabolic density
KW - Regional background
KW - Syncline
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U2 - 10.1016/j.cageo.2007.11.002
DO - 10.1016/j.cageo.2007.11.002
M3 - Article
AN - SCOPUS:43649108056
SN - 0098-3004
VL - 34
SP - 955
EP - 966
JO - Computers and Geosciences
JF - Computers and Geosciences
IS - 8
ER -