Gravity inversion for heterogeneous sedimentary basin with b-spline polynomial approximation using differential evolution algorithm

Arka Roy

doi:10.1190/GEO2019-0779.1

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Gravity inversion for heterogeneous sedimentary basin with b-spline polynomial approximation using differential evolution algorithm

2021-04-08

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Arka Roy *

Chandra Prakash Dubey

M. Hanuma Prasad

DOI：10.1190/GEO2019-0779.1

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Abstract

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We have developed a MATLAB-based inversion program, b-spline polynomial approximation using the differential evolution algorithm (SPODEA), to recover the concealed basement geometry under heterogeneous sedimentary basins. Earlier inversion techniques used the discretized subsurface interface topography into a grid of juxtaposed elementary prisms to estimate the basement depth of a basin. Such discretization leads to the failure of the depth profile continuity and requires a higher number of inversion parameters for achieving the desired accuracy. The novel approach of SPODEA overcomes such limitations of earlier inversion techniques. SPODEA is based on the segment-wise b-spline optimization technique to estimate the basement depth by using high-order polynomials. Moreover, it can achieve an optimal misfit with minimal parametric information, which reduces the computational expense. Our inversion approach uses the differential evolution algorithm, which provides real parametric optimization and uses b-splines for accurate estimation of continuous depth profiles. The efficiency of our algorithm was determined with two complex synthetic sedimentary basin models comprised of constant and depth-varying density distributions. Furthermore, the uncertainty analysis of our inversion technique is evaluated by incorporating white Gaussian noise into the synthetic models. Finally, the utility of SPODEA is evaluated by inverting gravity anomalies for two different real sedimentary basins. It produces geologically reasonable outcomes that are in close agreement with basement structures from previously reported results.

Keywords:

PARTICLE SWARM OPTIMIZATION

BASEMENT RELIEF

DENSITY CONTRAST

WAVELET TRANSFORM

3-D INVERSION

ANOMALIES

FIELD

UNCERTAINTY

COMPUTATION

EXPRESSION