Specially report how many separate conducting bodies you have resolved.
The initial model recommended is the halfspace with resistivity of 100 Om*m.
Please, try to invert simultaneously the whole data set. However, any subset of it can be used, if your code have some limitations or you feel that some components are excessive. You may submit several variants (give them names to refer) with proper indication what data are inverted. Don't forget to outline your best solution.
Describe the model you constructed in the form of two 2D arrays (one of estimated resistivity Ro(X,Z) and the second with a posteriori error d_Ro(X,Z)) with values for centers of 1x1 km cells in the area [20,140]x[0,120] km, i.e. for X = 20.5,1.0,139.5 and Z = 0.5,1.0,119.5.
Write each array into resulting ASCII file 2S1_M.RES row by row, rows separated by space line, each row is written 10 values per line in free format with values separated by space symbol.
Write 1D background (normal) section structure as an additional table - layer's number, its resistivity (Om*m) and thickness (km).
Sibmit final model responses in tables like input data in file 2S1_D.DTB or in J-format (but only those components, which were inverted) - these data are important to calculate unified data misfit functionals.
Other useful information could be the following: