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NEW ASPECTS IN THE INVERSION OF GRAVITY PROFILES BY POLYNOMIAL METHOD *
Author(s) -
BALDI P.
Publication year - 1981
Publication title -
geophysical prospecting
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.735
H-Index - 79
eISSN - 1365-2478
pISSN - 0016-8025
DOI - 10.1111/j.1365-2478.1981.tb01022.x
Subject(s) - inversion (geology) , geology , gemology , regional geology , gravity anomaly , polynomial , extension (predicate logic) , geodesy , telmatology , economic geology , engineering geology , geometry , geophysics , mineralogy , mathematics , mathematical analysis , hydrogeology , seismology , geotechnical engineering , computer science , petroleum engineering , tectonics , volcanism , oil field , programming language
A bstract The gravity anomaly caused by a deviation of a density interface that is of constant profile but finite extension (a so‐called 2 1/2‐dimensional structure) can be expressed in polynomial form that can be inverted. Numerical experiments with synthetic structures show the viability of this inversion method.

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