
TY  - JOUR
A1  - J. Heath, Philip 
T1  - The three-dimensional inversion of magnetic and gravity gradient tensor data
JF  - ASEG Extended Abstracts
JO  - ASEG Extended Abstracts
Y1  - 2003
VL  - 2003
IS  - 2
SP  - 1
EP  - 4
KW  - 
UR  - https://doi.org/10.1071/ASEG2003AB069 
N2  - Algorithms have been constructed in MATLAB for the inversion of potential field tensor (vector gradient) data using Monte Carlo and downhill simplex processes. Such algorithms have been used to invert artificially created data sets generated from simple geological structures, such as linear dykes and faults. Both magnetic and gravity tensor data can be examined using the algorithms. The algorithms have been tested over a range of depths, from metres to kilometres. They stop inversion once ideal parameters are obtained (RMS error equal to one), or can be altered to continue, in order to overfit the model. 
ER  -

