none
10.1190/geo20110388.1
Society of Exploration Geophysicists
Society of Exploration Geophysicists
186
56173005
5981
2021031006505000865
10.1190
20210310T19:06:35Z
20120622T23:51:13Z
71
GEOPHYSICS
GEOPHYSICS
00168033
19422156
07
01
2012
77
4
Robust 3D gravity gradient inversion by planting anomalous densities
Leonardo
Uieda
Observatório Nacional, Geophysics Department, Rio de Janeiro, Brazil..
Valéria C. F.
Barbosa
Observatório Nacional, Geophysics Department, Rio de Janeiro, Brazil..
We have developed a new gravity gradient inversion method for estimating a 3D densitycontrast distribution defined on a grid of rectangular prisms. Our method consists of an iterative algorithm that does not require the solution of an equation system. Instead, the solution grows systematically around userspecified prismatic elements, called “seeds,” with given density contrasts. Each seed can be assigned a different densitycontrast value, allowing the interpretation of multiple sources with different density contrasts and that produce interfering signals. In real world scenarios, some sources might not be targeted for the interpretation. Thus, we developed a robust procedure that neither requires the isolation of the signal of the targeted sources prior to the inversion nor requires substantial prior information about the nontargeted sources. In our iterative algorithm, the estimated sources grow by the accretion of prisms in the periphery of the current estimate. In addition, only the columns of the sensitivity matrix corresponding to the prisms in the periphery of the current estimate are needed for the computations. Therefore, the individual columns of the sensitivity matrix can be calculated on demand and deleted after an accretion takes place, greatly reducing the demand for computer memory and processing time. Tests on synthetic data show the ability of our method to correctly recover the geometry of the targeted sources, even when interfering signals produced by nontargeted sources are present. Inverting the data from an airborne gravity gradiometry survey flown over the iron ore province of Quadrilátero Ferrífero, southeastern Brazil, we estimated a compact iron ore body that is in agreement with geologic information and previous interpretations.
07
01
2012
G55
G66
10.1190/geo20110388.1
10.1190/geo20110388.1
https://library.seg.org/doi/10.1190/geo20110388.1

https://library.seg.org/doi/pdf/10.1190/geo20110388.1

http://geophysics.geoscienceworld.org/cgi/doi/10.1190/geo20110388.1
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